TY - JOUR A1 - Morandi, Bertrand A1 - Kail, Jochem A1 - Tödter, Anne A1 - Wolter, Christian A1 - Piegay, Herve T1 - Diverse Approaches to Implement and Monitor River Restoration BT - a Comparative Perspective in France and Germany JF - Environmental Management N2 - River restoration is a main emphasis of river management in European countries. Cross-national comparisons of its implementation are still rare in scientific literature. Based on French and German national censuses, this study compares river restoration practices and monitoring by analysing 102 French and 270 German projects. This comparison aims to draw a spatial and temporal framework of restoration practices in both countries to identify potential drivers of cross-national similarities and differences. The results underline four major trends: (1) a lag of almost 15 years in river restoration implementation between France and Germany, with a consequently higher share of projects in Germany than in France, (2) substantial similarities in restored reach characteristics, short reach length, small rivers, and in "agricultural" areas, (3) good correspondences between stressors identified and restoration measures implemented. Morphological alterations were the most important highlighted stressors. River morphology enhancement, especially instream enhancements, were the most frequently implemented restoration measures. Some differences exist in specific restoration practices, as river continuity restoration were most frequently implemented in French projects, while large wood introduction or channel re-braiding were most frequently implemented in German projects, and (4) some quantitative and qualitative differences in monitoring practices and a significant lack of project monitoring, especially in Germany compared to France. These similarities and differences between Germany and France in restoration application and monitoring possibly result from a complex set of drivers that might be difficult to untangle (e.g., environmental, technical, political, cultural). KW - River restoration KW - Project monitoring KW - Hydromorphologic alteration KW - Mitigation measures KW - France KW - Germany Y1 - 2017 U6 - https://doi.org/10.1007/s00267-017-0923-3 SN - 0364-152X SN - 1432-1009 VL - 60 SP - 931 EP - 946 PB - Springer CY - New York ER - TY - JOUR A1 - Huck, Stefan A1 - Wohlwend, Stephan A1 - Coimbra, Rute A1 - Christ, Nicolas A1 - Weissert, Helmut T1 - Disentangling shallow-water bulk carbonate carbon isotope archives with evidence for multi-stage diagenesis BT - an in-depth component-specific petrographic and geochemical study from Oman (mid-Cretaceous) JF - The depositional record N2 - Disentangling shallow‐water bulk carbonate carbon isotope archives into primary and diagenetic components is a notoriously difficult task and even diagenetically screened records often provide chemostratigraphic patterns that significantly differ from global signals. This is mainly caused by the polygenetic nature of shallow‐water carbonate substrates, local carbon cycle processes causing considerable neritic–pelagic isotope gradients and the presence of hiatal surfaces resulting in extremely low carbonate preservation rates. Provided here is an in‐depth petrographic and geochemical evaluation of different carbonate phases of a mid‐Cretaceous (Barremian–Aptian) shallow‐water limestone succession (Jabal Madar section) deposited on the tropical Arabian carbonate platform in Oman. The superposition of stable isotope signatures of identified carbonate phases causes a complex and often noisy bulk carbon isotope pattern. Blocky sparite cements filling intergranular pores and bioclastic voids evidence intermediate to (arguably) deep burial diagenetic conditions during their formation, owing to different timing or differential faulting promoting the circulation of fluids from variable sources. In contrast, sparite cements filling sub‐vertical veins reveal a rock‐buffered diagenetic fluid composition with an intriguing moderate enrichment in 13C, probably due to fractionation during pressure release in the context of the Miocene exhumation of the carbonate platform under study. The presence of abundant, replacive dedolomite in mud‐supported limestone samples forced negative carbon and oxygen isotope changes that are either associated with the thermal breakdown of organic matter in the deep burial realm or the expulsion of buried meteoric water in the intermediate burial realm. Notwithstanding the documented stratigraphically variable and often facies‐related impact of different diagenetic fluids on the bulk‐rock stable isotope signature, the identification of diagenetic end‐members defined δ13C and δ18O threshold values that allowed the most reliable ‘primary’ bulk carbon isotope signatures to be extracted. Most importantly, this approach exemplifies how to place regional shallow‐water stable isotope patterns with evidence for a complex multi‐stage diagenetic history into a supraregional or even global context. KW - Arabian carbonate platform KW - Barremian-Aptian KW - multi-stage diagenesis KW - shallow-water chemostratigraphy Y1 - 2017 U6 - https://doi.org/10.1002/dep2.35 SN - 2055-4877 VL - 3 SP - 233 EP - 257 PB - Wiley CY - Hoboken ER - TY - JOUR A1 - Milewski, Robert A1 - Chabrillat, Sabine A1 - Behling, Robert T1 - Analyses of Recent Sediment Surface Dynamic of a Namibian Kalahari Salt Pan Based on Multitemporal Landsat and Hyperspectral Hyperion Data JF - Remote Sensing N2 - This study combines spaceborne multitemporal and hyperspectral data to analyze the spatial distribution of surface evaporite minerals and changes in a semi-arid depositional environment associated with episodic flooding events, the Omongwa salt pan (Kalahari, Namibia). The dynamic of the surface crust is evaluated by a change-detection approach using the Iterative-reweighted Multivariate Alteration Detection (IR-MAD) based on the Landsat archive imagery from 1984 to 2015. The results show that the salt pan is a highly dynamic and heterogeneous landform. A change gradient is observed from very stable pan border to a highly dynamic central pan. On the basis of hyperspectral EO-1 Hyperion images, the current distribution of surface evaporite minerals is characterized using Spectral Mixture Analysis (SMA). Assessment of field and image endmembers revealed that the pan surface can be categorized into three major crust types based on diagnostic absorption features and mineralogical ground truth data. The mineralogical crust types are related to different zones of surface change as well as pan morphology that influences brine flow during the pan inundation and desiccation cycles. These combined information are used to spatially map depositional environments where the more dynamic halite crust concentrates in lower areas although stable gypsum and calcite/sepiolite crusts appear in higher elevated areas. KW - salt pan KW - playa KW - hyperspectral KW - multitemporal KW - change detection KW - evaporite minerals Y1 - 2016 U6 - https://doi.org/10.3390/rs9020170 SN - 2072-4292 VL - 9 IS - 2 PB - MDPI CY - Basel ER - TY - JOUR A1 - Bössenkool, Berry A1 - Bürger, Gerd A1 - Heistermann, Maik T1 - Effects of sample size on estimation of rainfall extremes at high temperatures JF - Natural hazards and earth system sciences N2 - High precipitation quantiles tend to rise with temperature, following the so-called Clausius-Clapeyron (CC) scaling. It is often reported that the CC-scaling relation breaks down and even reverts for very high temperatures. In our study, we investigate this reversal using observational climate data from 142 stations across Germany. One of the suggested meteorological explanations for the breakdown is limited moisture supply. Here we argue that, instead, it could simply originate from undersampling. As rainfall frequency generally decreases with higher temperatures, rainfall intensities as dictated by CC scaling are less likely to be recorded than for moderate temperatures. Empirical quantiles are conventionally estimated from order statistics via various forms of plotting position formulas. They have in common that their largest representable return period is given by the sample size. In small samples, high quantiles are underestimated accordingly. The small-sample effect is weaker, or disappears completely, when using parametric quantile estimates from a generalized Pareto distribution (GPD) fitted with L moments. For those, we obtain quantiles of rainfall intensities that continue to rise with temperature. Y1 - 2017 U6 - https://doi.org/10.5194/nhess-17-1623-2017 SN - 1561-8633 VL - 17 SP - 1623 EP - 1629 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Knapmeyer-Endrun, Brigitte A1 - Golombek, Matthew P. A1 - Ohrnberger, Matthias T1 - Rayleigh Wave Ellipticity Modeling and Inversion for Shallow Structure at the Proposed InSight Landing Site in Elysium Planitia, Mars JF - Space science reviews N2 - The SEIS (Seismic Experiment for Interior Structure) instrument onboard the InSight mission will be the first seismometer directly deployed on the surface of Mars. From studies on the Earth and the Moon, it is well known that site amplification in low-velocity sediments on top of more competent rocks has a strong influence on seismic signals, but can also be used to constrain the subsurface structure. Here we simulate ambient vibration wavefields in a model of the shallow sub-surface at the InSight landing site in Elysium Planitia and demonstrate how the high-frequency Rayleigh wave ellipticity can be extracted from these data and inverted for shallow structure. We find that, depending on model parameters, higher mode ellipticity information can be extracted from single-station data, which significantly reduces uncertainties in inversion. Though the data are most sensitive to properties of the upper-most layer and show a strong trade-off between layer depth and velocity, it is possible to estimate the velocity and thickness of the sub-regolith layer by using reasonable constraints on regolith properties. Model parameters are best constrained if either higher mode data can be used or additional constraints on regolith properties from seismic analysis of the hammer strokes of InSight’s heat flow probe HP3 are available. In addition, the Rayleigh wave ellipticity can distinguish between models with a constant regolith velocity and models with a velocity increase in the regolith, information which is difficult to obtain otherwise. KW - Mars KW - Interior KW - Seismology KW - Regoliths Y1 - 2017 U6 - https://doi.org/10.1007/s11214-016-0300-1 SN - 0038-6308 SN - 1572-9672 VL - 211 SP - 339 EP - 382 PB - Springer CY - Dordrecht ER - TY - JOUR A1 - Baumbach, Lukas A1 - Siegmund, Jonatan F. A1 - Mittermeier, Magdalena A1 - Donner, Reik Volker T1 - Impacts of temperature extremes on European vegetation during the growing season JF - Biogeosciences N2 - Temperature is a key factor controlling plant growth and vitality in the temperate climates of the mid-latitudes like in vast parts of the European continent. Beyond the effect of average conditions, the timings and magnitudes of temperature extremes play a particularly crucial role, which needs to be better understood in the context of projected future rises in the frequency and/or intensity of such events. In this work, we employ event coincidence analysis (ECA) to quantify the likelihood of simultaneous occurrences of extremes in daytime land surface temperature anomalies (LSTAD) and the normalized difference vegetation index (NDVI). We perform this analysis for entire Europe based upon remote sensing data, differentiating between three periods corresponding to different stages of plant development during the growing season. In addition, we analyze the typical elevation and land cover type of the regions showing significantly large event coincidences rates to identify the most severely affected vegetation types. Our results reveal distinct spatio-temporal impact patterns in terms of extraordinarily large co-occurrence rates between several combinations of temperature and NDVI extremes. Croplands are among the most frequently affected land cover types, while elevation is found to have only a minor effect on the spatial distribution of corresponding extreme weather impacts. These findings provide important insights into the vulnerability of European terrestrial ecosystems to extreme temperature events and demonstrate how event-based statistics like ECA can provide a valuable perspective on environmental nexuses. Y1 - 2017 U6 - https://doi.org/10.5194/bg-14-4891-2017 SN - 1726-4170 SN - 1726-4189 VL - 14 SP - 4891 EP - 4903 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Aichner, Bernhard A1 - Hilt, Sabine A1 - Perillon, Cecile A1 - Gillefalk, Mikael A1 - Sachse, Dirk T1 - Biosynthetic hydrogen isotopic fractionation factors during lipid synthesis in submerged aquatic macrophytes: Effect of groundwater discharge and salinity JF - Organic geochemistry : the international journal for rapid publication of current research in organic geochemistry and biochemistry N2 - Sedimentary lipid biomarkers have become widely used tools for reconstructing past climatic and ecological changes due to their ubiquitous occurrence in lake sediments. In particular, the hydrogen isotopic composition (expressed as delta D values) of leaf wax lipids derived from terrestrial plants has been a focus of research during the last two decades and the understanding of competing environmental and plant physiological factors influencing the delta D values has greatly improved. Comparatively less attention has been paid to lipid biomarkers derived from aquatic plants, although these compounds are abundant in many lacustrine sediments. We therefore conducted a field and laboratory experiment to study the effect of salinity and groundwater discharge on the isotopic composition of aquatic plant biomarkers. We analyzed samples of the common submerged plant species, Potamogeton pectinatus (sago pondweed), which has a wide geographic distribution and can tolerate high salinity. We tested the effect of groundwater discharge (characterized by more negative delta D values relative to lake water) and salinity on the delta D values of n-alkanes from P. pectinatus by comparing plants (i) collected from the oligotrophic freshwater Lake Stechlin (Germany) at shallow littoral depth from locations with and without groundwater discharge, and (ii) plants grown from tubers collected from the eutrophic Lake Muggelsee in nutrient solution at four salinity levels. Isotopically depleted groundwater did not have a significant influence on the delta D values of n-alkanes in Lake Stechlin P. pectinatus and calculated isotopic fractionation factors epsilon(l/w) between lake water and n-alkanes averaged -137 +/- 9%(n-C-23), -136 +/- 7%(n-C-25) and -131 +/- 6%(n-C-27), respectively. Similar epsilon values were calculated for plants from Lake Muggelsee grown in freshwater nutrient solution (-134 +/- 11% for n-C-23), while greater fractionation was observed at increased salinity values of 10 (163 +/- 12%) and 15(-172 +/- 15%). We therefore suggest an average e value of -136 +/- 9% between source water and the major n-alkanes in P. pectinatus grown under freshwater conditions. Our results demonstrate that isotopic fractionation can increase by 30-40% at salinity values 10 and 15. These results could be explained either by inhibited plant growth at higher salinity, or by metabolic adaptation to salt stress that remain to be elucidated. A potential salinity effect on dD values of aquatic lipids requires further examination, since this would impact on the interpretation of downcore isotopic data in paleohydrologic studies. (C) 2017 Elsevier Ltd. All rights reserved. Y1 - 2017 U6 - https://doi.org/10.1016/j.orggeochem.2017.07.021 SN - 0146-6380 VL - 113 SP - 10 EP - 16 PB - Elsevier CY - Oxford ER - TY - JOUR A1 - Steinhöfel, Grit A1 - Breuer, Jörn A1 - von Blanckenburg, Friedhelm A1 - Horn, Ingo A1 - Sommer, Michael T1 - The dynamics of Si cycling during weathering in two small catchments in the Black Forest (Germany) traced by Si isotopes JF - Chemical geology : official journal of the European Association for Geochemistry N2 - Silicon stable isotopes have emerged as a powerful proxy to investigate weathering because Si uptake from solution by secondary minerals or by the vegetation causes significant shifts in the isotope composition. In this study, we determined the Si isotope compositions of the principle Si pools within two small catchments located on sandstone and paragneiss, respectively, in the temperate Black Forest (Germany). At both settings, clay formation is dominated by mineral transformation preserving largely the signature of parental minerals with delta Si-30 values of around -0.7%. Bulk soils rich in primary minerals are similar to bulk parental material with delta Si-30 values close to -0.4%. Topsoils are partly different because organic matter degradation has promoted intense weathering leading to delta Si-30 values as low as -1.0%. Water samples expose highly dynamic weathering processes in the soil zone: 1) after spring snowmelt, increased release of DOC and high water fluxes trigger clay mineral dissolution which leads to delta Si-30 values down to -0.7% and 2) in course of the summer, Si uptake by the vegetation and secondary mineral formation drives dissolved Si to typical positive delta Si-30 values up to 1.1%. Groundwater with delta Si-30 values of around 0.4% records steady processes in bedrock reflecting plagioclase weathering together with kaolinite precipitation. An isotope mass balance approach reveals incongruent weathering conditions where denudation of Si is largely driven by physical erosion. Erosion of phytoliths contributes 3 to 21% to the total Si export flux, which is in the same order as the dissolved Si flux. These results elucidate the Si dynamics during weathering on catchments underlain of sedimentary origin, prevailing on the Earth surface and provide therefore valuable information to interpret the isotope signature of large river systems. KW - Weathering KW - Sedimentary rocks KW - Biogeochemical Si cycle KW - Silicon isotopes KW - UV femtosecond laser ablation Y1 - 2017 U6 - https://doi.org/10.1016/j.chemgeo.2017.06.026 SN - 0009-2541 SN - 1878-5999 VL - 466 SP - 389 EP - 402 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Brune, Sascha A1 - Corti, Giacomo A1 - Ranalli, Giorgio T1 - Controls of inherited lithospheric heterogeneity on rift linkage: Numerical and analog models of interaction between the Kenyan and Ethiopian rifts across the Turkana depression JF - Tectonics N2 - Inherited rheological structures in the lithosphere are expected to have large impact on the architecture of continental rifts. The Turkana depression in the East African Rift connects the Main Ethiopian Rift to the north with the Kenya rift in the south. This region is characterized by a NW-SE trending band of thinned crust inherited from a Mesozoic rifting event, which is cutting the present-day N-S rift trend at high angle. In striking contrast to the narrow rifts in Ethiopia and Kenya, extension in the Turkana region is accommodated in subparallel deformation domains that are laterally distributed over several hundred kilometers. We present both analog experiments and numerical models that reproduce the along-axis transition from narrow rifting in Ethiopia and Kenya to a distributed deformation within the Turkana depression. Similarly to natural observations, our models show that the Ethiopian and Kenyan rifts bend away from each other within the Turkana region, thus forming a right-lateral step over and avoiding a direct link to form a continuous N-S depression. The models reveal five potential types of rift linkage across the preexisting basin: three types where rifts bend away from the inherited structure connecting via a (1) wide or (2) narrow rift or by (3) forming a rotating microplate, (4) a type where rifts bend towards it, and (5) straight rift linkage. The fact that linkage type 1 is realized in the Turkana region provides new insights on the rheological configuration of the Mesozoic rift system at the onset of the recent rift episode. Plain Language Summary The Turkana depression in the Kenya/Ethiopia borderland is most famous for its several million years old human fossils, but it also holds a rich geological history of continental separation. The Turkana region is a lowland located between the East African and Ethiopian domes because its crust and mantle have been stretched in a continent-wide rift event during Cretaceous times about 140-120 Ma ago. This thin lithosphere exerted paramount control on the dynamics of East African rifting in this area, which commenced around 15 Ma ago and persists until today. Combining analog "sandbox" experiments with numerical geodynamic modeling, we find that inherited rift structures explain the dramatic change in rift style from deep, narrow rift basins north and south of the Turkana area to wide, distributed deformation within the Turkana depression. The failed Cretaceous rift is also responsible for the eastward bend of the Ethiopian rift and the westward bend of the Kenyan rift when entering the Turkana depression, which generated the characteristic hook-shaped form of present-day Lake Turkana. Combing two independent modeling techniques-analog and numerical experiments-is a very promising approach allowing to draw robust conclusions about the processes that shape the surface of our planet. KW - continental rifting KW - east African rift KW - numerical modeling KW - analog modeling KW - tectonic inheritance KW - Turkana depression Y1 - 2017 U6 - https://doi.org/10.1002/2017TC004739 SN - 0278-7407 SN - 1944-9194 VL - 36 SP - 1767 EP - 1786 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Boers, Niklas A1 - Goswami, Bedartha A1 - Ghil, Michael T1 - A complete representation of uncertainties in layer-counted paleoclimatic archives JF - Climate of the past : an interactive open access journal of the European Geosciences Union N2 - Accurate time series representation of paleoclimatic proxy records is challenging because such records involve dating errors in addition to proxy measurement errors. Rigorous attention is rarely given to age uncertainties in paleoclimatic research, although the latter can severely bias the results of proxy record analysis. Here, we introduce a Bayesian approach to represent layer-counted proxy records - such as ice cores, sediments, corals, or tree rings - as sequences of probability distributions on absolute, error-free time axes. The method accounts for both proxy measurement errors and uncertainties arising from layer-counting-based dating of the records. An application to oxygen isotope ratios from the North Greenland Ice Core Project (NGRIP) record reveals that the counting errors, although seemingly small, lead to substantial uncertainties in the final representation of the oxygen isotope ratios. In particular, for the older parts of the NGRIP record, our results show that the total uncertainty originating from dating errors has been seriously underestimated. Our method is next applied to deriving the overall uncertainties of the Suigetsu radiocarbon comparison curve, which was recently obtained from varved sediment cores at Lake Suigetsu, Japan. This curve provides the only terrestrial radiocarbon comparison for the time interval 12.5-52.8 kyr BP. The uncertainties derived here can be readily employed to obtain complete error estimates for arbitrary radiometrically dated proxy records of this recent part of the last glacial interval. Y1 - 2017 U6 - https://doi.org/10.5194/cp-13-1169-2017 SN - 1814-9324 SN - 1814-9332 VL - 13 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Rach, Oliver A1 - Engels, S. A1 - Kahmen, A. A1 - Brauer, Achim A1 - Martin-Puertas, C. A1 - van Geel, B. A1 - Sachse, Dirk T1 - Hydrological and ecological changes in western Europe between 3200 and 2000 years BP derived from lipid biomarker delta D values in lake Meerfelder Maar sediments JF - Quaternary science reviews : the international multidisciplinary research and review journal N2 - One of the most significant Late Holocene climate shifts occurred around 2800 years ago, when cooler and wetter climate conditions established in western Europe. This shift coincided with an abrupt change in regional atmospheric circulation between 2760 and 2560 cal years BP, which has been linked to a grand solar minimum with the same duration (the Homeric Minimum). We investigated the temporal sequence of hydroclimatic and vegetation changes across this interval of climatic change (Homeric climate oscillation) by using lipid biomarker stable hydrogen isotope ratios (ED values) and pollen assemblages from the annually-laminated sediment record from lake Meerfelder Maar (Germany). Over the investigated interval (3200-2000 varve years BP), terrestrial lipid biomarker ED showed a gradual trend to more negative values, consistent with the western Europe long-term climate trend of the Late Holocene. At ca. 2640 varve years BP we identified a strong increase in aquatic plants and algal remains, indicating a rapid change in the aquatic ecosystem superimposed on this long-term trend. Interestingly, this aquatic ecosystem change was accompanied by large changes in ED values of aquatic lipid biomarkers, such as nC(21) and nC(23) (by between 22 and 30%(0)). As these variations cannot solely be explained by hydroclimate changes, we suggest that these changes in the Wag value were influenced by changes in n-alkane source organisms. Our results illustrate that if ubiquitous aquatic lipid biomarkers are derived from a limited pool of organisms, changes in lake ecology can be a driving factor for variations on sedimentary lipid MN values, which then could be easily misinterpreted in terms of hydro climatic changes. (C) 2017 Elsevier Ltd. All rights reserved. KW - Holocene KW - Climate dynamics KW - Paleoclimatology KW - Western Europe KW - Continental biomarkers KW - Organic geochemistry KW - Stable isotopes KW - Vegetation dynamics Y1 - 2017 U6 - https://doi.org/10.1016/j.quascirev.2017.07.019 SN - 0277-3791 VL - 172 SP - 44 EP - 54 PB - Elsevier CY - Oxford ER - TY - JOUR A1 - Rubey, Michael A1 - Brune, Sascha A1 - Heine, Christian A1 - Davies, D. Rhodri A1 - Williams, Simon E. A1 - Müller, R. Dietmar T1 - role of subducted slabs JF - Solid earth Y1 - 2017 U6 - https://doi.org/10.5194/se-8-899-2017 SN - 1869-9510 SN - 1869-9529 VL - 8 SP - 899 EP - 919 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Bürger, Gerhard T1 - On trend detection JF - Hydrological processes N2 - A main obstacle to trend detection in time series occurs when they are autocorrelated. By reducing the effective sample size of a series, autocorrelation leads to decreased trend significance. Numerous recipes attempt to mitigate the effect of autocorrelation, either by adjusting for the reduced effective sample size or by removing the autocorrelated components of a series. This short note deals with the latter, also called prewhitening (PW). It is known that removal of autocorrelation also removes part of the trend, which may affect the signal-to-noise ratio. Two popular methods have dealt with this problem, the trend-free prewhitening (TFPW) and the iterative prewhitening. Although it is generally accepted that both methods reduce the adverse effects of PW on the trend magnitude, corresponding effects on statistical significance have not been clearly stated for TFPW. Using a Monte Carlo approach, it is demonstrated that both methods entail quite different Type-I error rates. The iterative prewhitening produces rates that are generally close to the nominal significance level. The TFPW, however, shows very high Type-I error rates with increasing autocorrelation. The corresponding rate of false trend detections is unacceptable for applications, so that published trends based on TFPW need to be reassessed. KW - autocorrelation KW - trend significance KW - Type-I error Y1 - 2017 U6 - https://doi.org/10.1002/hyp.11280 SN - 0885-6087 SN - 1099-1085 VL - 31 SP - 4039 EP - 4042 PB - Wiley CY - Hoboken ER - TY - JOUR A1 - Nazarova, Larisa B. A1 - Bleibtreu, Annette A1 - Hoff, Ulrike A1 - Dirksen, Veronika A1 - Diekmann, Bernhard T1 - Changes in temperature and water depth of a small mountain lake during the past 3000 years in Central Kamchatka reflected by a chironomid record JF - Quaternary international : the journal of the International Union for Quaternary Research N2 - We investigated chironomid assemblages of a well-dated sediment core from a small seepage lake situated at the eastern slope of the Central Kamchatka Mountain Chain, Far East Russia. The chironomid fauna of the investigated Sigrid Lake is dominated by littoral taxa that are sensitive to fluctuations of the water level. Two groups of taxa interchangeably dominate the record responding to the changes in the lake environment during the past 2800 years. The first group of littoral phytophilic taxa includes Psectrocladius sordidellus-type, Corynoneura arctica-type and Dicrotendipes nervosus-type. The abundances of the taxa from this group have the strongest influence on the variations of PCA 1, and these taxa mostly correspond to low water levels, moderate temperatures and slightly acidified conditions. The second group of taxa includes Microtendipes pedellus-type, Tanytarsus lugens-type, and Tanytarsus pallidicornistype. The variations in the abundances of these taxa, and especially of M. pedellus-type, are in accordance with PCA 2 and correspond to the higher water level in the lake, more oligotrophic and neutral pH conditions. Water depths (WD) were reconstructed, using a modern chironomid-based temperature and water depth calibration data set (training set) and inference model from East Siberia (Nazarova et al., 2011). Mean July air temperatures (T July) were inferred using a chironomid-based temperature inference model based on a modern calibration data set for the Far East (Nazarova et al., 2015). The application of transfer functions resulted in reconstructed T July fluctuations of approximately 3 degrees C over the last 2800 years. Low temperatures (11.0-12.0 degrees C) were reconstructed for the periods between ca 1700 and 1500 cal yr BP (corresponding to the Kofun cold stage) and between ca 1200 and 150 cal yr BP (partly corresponding to the Little Ice Age [LIA]). Warm periods (modern T July or higher) were reconstructed for the periods between ca 2700 and 1800 cal yr BP, 1500 and 1300 cal yr BP and after 150 cal yr BP. WD reconstruction revealed that the lake level was lower than its present level at the beginning of the record between ca 2600 and 2300 cal yr BP and ca 550 cal yr BP. Between ca 2300 and 700 cal yr BP as well as between 450 and 150 cal yr BP, the lake level was higher than it is today, most probably reflecting more humid conditions. (C) 2016 Elsevier Ltd and INQUA. All rights reserved. KW - Kamchatka KW - Chironomids KW - Palaeoclimate KW - Late Holocene KW - Temperature KW - Water depth Y1 - 2017 U6 - https://doi.org/10.1016/j.quaint.2016.10.008 SN - 1040-6182 SN - 1873-4553 VL - 447 SP - 46 EP - 58 PB - Elsevier CY - Oxford ER - TY - JOUR A1 - Negi, Sanjay S. A1 - Paul, Ajay A1 - Cesca, Simone A1 - Kamal, A1 - Kriegerowski, Marius A1 - Mahesh, P. A1 - Gupta, Sandeep T1 - Crustal velocity structure and earthquake processes of Garhwal-Kumaun Himalaya: Constraints from regional waveform inversion and array beam modeling JF - Tectonophysics : international journal of geotectonics and the geology and physics of the interior of the earth N2 - In order to understand present day earthquake kinematics at the Indian plate boundary, we analyse seismic broadband data recorded between 2007 and 2015 by the regional network in the Garhwal-Kumaun region, northwest Himalaya. We first estimate a local 1-D velocity model for the computation of reliable Green's functions, based on 2837 P-wave and 2680 S-wave arrivals from 251 well located earthquakes. The resulting 1-D crustal structure yields a 4-layer velocity model down to the depths of 20 km. A fifth homogeneous layer extends down to 46 km, constraining the Moho using travel-time distance curve method. We then employ a multistep moment tensor (MT) inversion algorithm to infer seismic moment tensors of 11 moderate earthquakes with Mw magnitude in the range 4.0–5.0. The method provides a fast MT inversion for future monitoring of local seismicity, since Green's functions database has been prepared. To further support the moment tensor solutions, we additionally model P phase beams at seismic arrays at teleseismic distances. The MT inversion result reveals the presence of dominant thrust fault kinematics persisting along the Himalayan belt. Shallow low and high angle thrust faulting is the dominating mechanism in the Garhwal-Kumaun Himalaya. The centroid depths for these moderate earthquakes are shallow between 1 and 12 km. The beam modeling result confirm hypocentral depth estimates between 1 and 7 km. The updated seismicity, constrained source mechanism and depth results indicate typical setting of duplexes above the mid crustal ramp where slip is confirmed along out-of-sequence thrusting. The involvement of Tons thrust sheet in out-of-sequence thrusting indicate Tons thrust to be the principal active thrust at shallow depth in the Himalayan region. Our results thus support the critical taper wedge theory, where we infer the microseismicity cluster as a result of intense activity within the Lesser Himalayan Duplex (LHD) system. KW - Critical taper wedge KW - Lesser Himalayan Duplex KW - Out-of-sequence thrust Y1 - 2017 U6 - https://doi.org/10.1016/j.tecto.2017.05.007 SN - 0040-1951 SN - 1879-3266 VL - 712 SP - 45 EP - 63 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Markovic, Danijela A1 - Carrizo, Savrina F. A1 - Kaercher, Oskar A1 - Walz, Ariane A1 - David, Jonathan N. W. T1 - Vulnerability of European freshwater catchments to climate change JF - Global change biology N2 - Climate change is expected to exacerbate the current threats to freshwater ecosystems, yet multifaceted studies on the potential impacts of climate change on freshwater biodiversity at scales that inform management planning are lacking. The aim of this study was to fill this void through the development of a novel framework for assessing climate change vulnerability tailored to freshwater ecosystems. The three dimensions of climate change vulnerability are as follows: (i) exposure to climate change, (ii) sensitivity to altered environmental conditions and (iii) resilience potential. Our vulnerability framework includes 1685 freshwater species of plants, fishes, molluscs, odonates, amphibians, crayfish and turtles alongside key features within and between catchments, such as topography and connectivity. Several methodologies were used to combine these dimensions across a variety of future climate change models and scenarios. The resulting indices were overlaid to assess the vulnerability of European freshwater ecosystems at the catchment scale (18 783 catchments). The Balkan Lakes Ohrid and Prespa and Mediterranean islands emerge as most vulnerable to climate change. For the 2030s, we showed a consensus among the applied methods whereby up to 573 lake and river catchments are highly vulnerable to climate change. The anthropogenic disruption of hydrological habitat connectivity by dams is the major factor reducing climate change resilience. A gap analysis demonstrated that the current European protected area network covers <25% of the most vulnerable catchments. Practical steps need to be taken to ensure the persistence of freshwater biodiversity under climate change. Priority should be placed on enhancing stakeholder cooperation at the major basin scale towards preventing further degradation of freshwater ecosystems and maintaining connectivity among catchments. The catchments identified as most vulnerable to climate change provide preliminary targets for development of climate change conservation management and mitigation strategies. KW - catchment connectivity KW - climate change KW - exposure KW - freshwater biodiversity KW - gap analysis KW - resilience KW - sensitivity KW - vulnerability Y1 - 2017 U6 - https://doi.org/10.1111/gcb.13657 SN - 1354-1013 SN - 1365-2486 VL - 23 SP - 3567 EP - 3580 PB - Wiley CY - Hoboken ER - TY - JOUR A1 - Egholm, David L. A1 - Jansen, John D. A1 - Braedstrup, Christian F. A1 - Pedersen, Vivi K. A1 - Andersen, Jane Lund A1 - Ugelvig, Sofie V. A1 - Larsen, Nicolaj K. A1 - Knudsen, Mads F. T1 - Formation of plateau landscapes on glaciated continental margins JF - Nature geoscience N2 - Low-relief plateaus separated by deeply incised fjords are hallmarks of glaciated, passive continental margins. Spectacular examples fringe the once ice-covered North Atlantic coasts of Greenland, Norway and Canada, but low-relief plateau landscapes also underlie present-day ice sheets in Antarctica and Greenland. Dissected plateaus have long been viewed as the outcome of selective linear erosion by ice sheets that focus incision in glacial troughs, leaving the intervening landscapes essentially unaffected. According to this hypothesis, the plateaus are remnants of preglacial low-relief topography. However, here we use computational experiments to show that, like fjords, plateaus are emergent properties of long-term ice-sheet erosion. Ice sheets can either increase or decrease subglacial relief depending on the wavelength of the underlying topography, and plateau topography arises dynamically from evolving feedbacks between topography, ice dynamics and erosion over million-year timescales. This new mechanistic explanation for plateau formation opens the possibility of plateaus contributing significantly to accelerated sediment flux at the onset of the late Cenozoic glaciations, before becoming stable later in the Quaternary. Y1 - 2017 U6 - https://doi.org/10.1038/NGEO2980 SN - 1752-0894 SN - 1752-0908 VL - 10 SP - 592 EP - + PB - Nature Publ. Group CY - New York ER - TY - JOUR A1 - Neill, Christopher A1 - Jankowski, KathiJo A1 - Brando, Paulo M. A1 - Coe, Michael T. A1 - Deegan, Linda A. A1 - Macedo, Marcia N. A1 - Riskin, Shelby H. A1 - Porder, Stephen A1 - Elsenbeer, Helmut A1 - Krusche, Alex V. T1 - Surprisingly Modest Water Quality Impacts From Expansion and Intensification of Large-Sscale Commercial Agriculture in the Brazilian Amazon-Cerrado Region JF - Tropical conservation science N2 - Large-scale commercial cropping of soybeans expanded in the tropical Amazon and Cerrado biomes of Brazil after 1990. More recently, cropping intensified from single-cropping of soybeans to double-cropping of soybeans with corn or cotton. Cropland expansion and intensification, and the accompanying use of mineral fertilizers, raise concerns about whether nutrient runoff and impacts to surface waters will be similar to those experienced in commercial cropland regions at temperate latitudes. We quantified water infiltration through soils, water yield, and streamwater chemistry in watersheds draining native tropical forest and single-and double-cropped areas on the level, deep, highly weathered soils where cropland expansion and intensification typically occurs. Although water yield increased four-fold from croplands, streamwater chemistry remained largely unchanged. Soil characteristics exerted important control over the movement of nitrogen (N) and phosphorus (P) into streams. High soil infiltration rates prevented surface erosion and movement of particulate P, while P fixation in surface soils restricted P movement to deeper soil layers. Nitrogen retention in deep soils, likely by anion exchange, also appeared to limit N leaching and export in streamwater from both single-and double-cropped watersheds that received nitrogen fertilizer. These mechanisms led to lower streamwater P and N concentrations and lower watershed N and P export than would be expected, based on studies from temperate croplands with similar cropping and fertilizer application practices. KW - water KW - quality KW - agriculture KW - intensification KW - impact Y1 - 2017 U6 - https://doi.org/10.1177/1940082917720669 SN - 1940-0829 VL - 10 PB - Sage Publ. CY - Thousand Oaks ER - TY - JOUR A1 - Stinnesbeck, Wolfgang A1 - Becker, Julia A1 - Hering, Fabio A1 - Frey, Eberhard A1 - Gonzalez Gonzalez, Arturo A1 - Fohlmeister, Jens Bernd A1 - Stinnesbeck, Sarah A1 - Frank, Norbert A1 - Terrazas Mata, Alejandro A1 - Elena Benavente, Martha A1 - Aviles Olguin, Jeronimo A1 - Aceves Nunez, Eugenio A1 - Zell, Patrick A1 - Deininger, Michael T1 - The earliest settlers of Mesoamerica date back to the late Pleistocene JF - PLoS one N2 - Preceramic human skeletal remains preserved in submerged caves near Tulum in the Mexican state of Quintana Roo, Mexico, reveal conflicting results regarding C-14 dating. Here we use U-series techniques for dating a stalagmite overgrowing the pelvis of a human skeleton discovered in the submerged Chan Hol cave. The oldest closed system U/Th age comes from around 21 mm above the pelvis defining the terminus ante quem for the pelvis to 11311 +/- 370 y BP. However, the skeleton might be considerable older, probably as old as 13 ky BP as indicated by the speleothem stable isotope data. The Chan Hol individual confirms a late Pleistocene settling of Mesoamerica and represents one of the oldest human osteological remains in America. Y1 - 2017 U6 - https://doi.org/10.1371/journal.pone.0183345 SN - 1932-6203 VL - 12 PB - PLoS CY - San Fransisco ER - TY - JOUR A1 - Kornhuber, Kai A1 - Petoukhov, Vladimir A1 - Karoly, D. A1 - Petri, Stefan A1 - Rahmstorf, Stefan A1 - Coumou, Dim T1 - Summertime Planetary Wave Resonance in the Northern and Southern Hemispheres JF - Journal of climate Y1 - 2017 U6 - https://doi.org/10.1175/JCLI-D-16-0703.1 SN - 0894-8755 SN - 1520-0442 VL - 30 SP - 6133 EP - 6150 PB - American Meteorological Soc. CY - Boston ER - TY - JOUR A1 - Schmidt, Katja A1 - Walz, Ariane A1 - Martin-Lopez, Berta A1 - Sachse, Rene T1 - Testing socio-cultural valuation methods of ecosystem services to explain land use preferences JF - Ecosystem Services : Science, Policy and Practice N2 - Socio-cultural valuation still emerges as a methodological field in ecosystem service (ES) research and until now lacks consistent formalisation and balanced application in ES assessments. In this study, we examine the explanatory value of ES values for land use preferences. We use 563 responses to a survey about the Pentland Hills regional park in Scotland. Specifically, we aim to (1) identify clusters of land use preferences by using a novel visualisation tool, (2) test if socio-cultural values of ESs or (3) user characteristics are linked with land use preferences, and (4) determine whether both socio-cultural values of ESs and user characteristics can predict land use preferences. Our results suggest that there are five groups of people with different land use preferences, ranging from forest and nature enthusiasts to traditionalists, multi-functionalists and recreation seekers. Rating and weighting of ESs and user characteristics were associated with different clusters. Neither socio-cultural values nor user characteristics were suitable predictors for land use preferences. While several studies have explored land use preferences by identifying socio-cultural values in the past, our findings imply that in this case study ES values inform about general perceptions but do not replace the assessment of land use preferences. (C) 2017 The Authors. Published by Elsevier B.V. This is an open access article under the CC BY-NC-ND license. KW - Non-monetary valuation KW - Values KW - Visitors KW - Landscape visualisation KW - Visualisation tool Y1 - 2017 U6 - https://doi.org/10.1016/j.ecoser.2017.07.001 SN - 2212-0416 VL - 26 SP - 270 EP - 288 PB - Elsevier CY - Amsterdam ER - TY - GEN A1 - Zöller, Gert T1 - Comment on "Estimation of Earthquake Hazard Parameters from Incomplete Data Files. Part III. Incorporation of Uncertainty of Earthquake-Occurrence Model" by Andrzej Kijko, Ansie Smit, and Markvard A. Sellevoll T2 - Bulletin of the Seismological Society of America N2 - Kijko et al. (2016) present various methods to estimate parameters that are relevant for probabilistic seismic-hazard assessment. One of these parameters, although not the most influential, is the maximum possible earthquake magnitude m(max). I show that the proposed estimation of m(max) is based on an erroneous equation related to a misuse of the estimator in Cooke (1979) and leads to unstable results. So far, reported finite estimations of m(max) arise from data selection, because the estimator in Kijko et al. (2016) diverges with finite probability. This finding is independent of the assumed distribution of earthquake magnitudes. For the specific choice of the doubly truncated Gutenberg-Richter distribution, I illustrate the problems by deriving explicit equations. Finally, I conclude that point estimators are generally not a suitable approach to constrain m(max). Y1 - 2017 U6 - https://doi.org/10.1785/0120160193 SN - 0037-1106 SN - 1943-3573 VL - 107 SP - 1975 EP - 1978 PB - Seismological Society of America CY - Albany ER - TY - JOUR A1 - Hua, Quan A1 - Cook, Duncan A1 - Fohlmeister, Jens Bernd A1 - Penny, Dan A1 - Bishop, Paul A1 - Buckman, Solomon T1 - Radiocarbon Dating of a Speleothem Record of Paleoclimate for Angkor, Cambodia JF - Radiocarbon : an international journal of cosmogenic isotope research N2 - We report the chronological construction for the top portion of a speleothem, PC1, from southern Cambodia with the aim of reconstructing a continuous high-resolution climate record covering the fluorescence and decline of the medieval Khmer kingdom and its capital at Angkor (similar to 9th-15th centuries AD). Earlier attempts to date PC1 by the standard U-Th method proved unsuccessful. We have therefore dated this speleothem using radiocarbon. Fifty carbonate samples along the growth axis of PC1 were collected for accelerator mass spectrometry (AMS) analysis. Chronological reconstruction for PC1 was achieved using two different approaches described by Hua et al. (2012a) and Lechleitner et al. (2016a). Excellent concordance between the two age-depth models indicates that the top similar to 47 mm of PC1 grew during the last millennium with a growth hiatus during similar to 1250-1650 AD, resulting from a large change in measured C-14 values at 34.4-35.2 mm depth. The timing of the growth hiatus covers the period of decades-long droughts during the 14th-16th centuries AD indicated in regional climate records. KW - Angkor KW - chronological construction KW - radiocarbon KW - Southeast Asia KW - tropical speleothems Y1 - 2017 U6 - https://doi.org/10.1017/RDC.2017.115 SN - 0033-8222 SN - 1945-5755 VL - 59 IS - Special Issue 6 / 2 SP - 1873 EP - 1890 PB - The University of Arizona, Department of Geosciences CY - Tucson, Ariz. ER - TY - JOUR A1 - Bernardez, Patricia A1 - Prego, Ricardo A1 - Virginia Filgueiras, Ana A1 - Ospina-Alvarez, Natalia A1 - Santos-Echeandia, Juan A1 - Angel Alvarez-Vazquez, Miguel A1 - Caetano, Miguel T1 - Lithogenic sources, composition and intra-annual variability of suspended particulate matter supplied from rivers to the Northern Galician Rias (Bay of Biscay) JF - Journal of sea research N2 - Scarce research about small European rivers from non-human impacted areas to determine their natural background state has been undertaken. During the annual hydrological cycle of 2008-9 the patterns of particulate supply (SPM, POC, PON, Al, Cd, Co, Cr, Cu, Fe, Ni, Pb, V, Zn) from the rivers Sor, Mera Landro, Lourido and Landoi to the Northern Galician Rias (SW Bay of Biscay) were tackled. No differences in the composition of the SPM were detected for the studied rivers regarding Al, Fe and POC but the relative percentage of particulate trace elements (PTE) discriminate the rivers. So, Cr, Co and Ni in the Lourido, and Landoi rivers, and Cu in the Mera River, are controlled by watershed minerals of Ortegal Geological Complex while for the rest rivers PTE are by granitic and Ollo de Sapo bedrock watershed. Therefore, the imprint of PTE in the parental rocks of the river basins is reflected on the coastal sediments of the Rias. The main process controlling the dynamics and variations of chemical elements in the particulate form is the river discharge. This fact exemplifies that these rivers presents a natural behavior not being highly influenced by anthropogenic activities. KW - SPM KW - Trace metals KW - Organic matter KW - River KW - W Cantabrian coast Y1 - 2017 U6 - https://doi.org/10.1016/j.seares.2017.05.006 SN - 1385-1101 SN - 1873-1414 VL - 130 SP - 73 EP - 84 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Weisshuhn, Peter A1 - Reckling, Moritz A1 - Stachow, Ulrich A1 - Wiggering, Hubert T1 - Supporting Agricultural Ecosystem Services through the Integration of Perennial Polycultures into Crop Rotations JF - Sustainability N2 - This review analyzes the potential role and long-term effects of field perennial polycultures (mixtures) in agricultural systems, with the aim of reducing the trade-offs between provisioning and regulating ecosystem services. First, crop rotations are identified as a suitable tool for the assessment of the long-term effects of perennial polycultures on ecosystem services, which are not visible at the single-crop level. Second, the ability of perennial polycultures to support ecosystem services when used in crop rotations is quantified through eight agricultural ecosystem services. Legume-grass mixtures and wildflower mixtures are used as examples of perennial polycultures, and compared with silage maize as a typical crop for biomass production. Perennial polycultures enhance soil fertility, soil protection, climate regulation, pollination, pest and weed control, and landscape aesthetics compared with maize. They also score lower for biomass production compared with maize, which confirms the trade-off between provisioning and regulating ecosystem services. However, the additional positive factors provided by perennial polycultures, such as reduced costs for mineral fertilizer, pesticides, and soil tillage, and a significant preceding crop effect that increases the yields of subsequent crops, should be taken into account. However, a full assessment of agricultural ecosystem services requires a more holistic analysis that is beyond the capabilities of current frameworks. KW - agroecosystem KW - assessment KW - legume-grass mixture KW - wildflower mixture KW - perennial crop KW - mixed cropping Y1 - 2017 U6 - https://doi.org/10.3390/su9122267 SN - 2071-1050 VL - 9 PB - MDPI CY - Basel ER - TY - JOUR A1 - Totz, Sonja Juliana A1 - Tziperman, Eli A1 - Coumou, Dim A1 - Pfeiffer, Karl A1 - Cohen, Judah T1 - Winter precipitation forecast in the European and mediterranean regions using cluster analysis JF - Geophysical research letters N2 - The European climate is changing under global warming, and especially the Mediterranean region has been identified as a hot spot for climate change with climate models projecting a reduction in winter rainfall and a very pronounced increase in summertime heat waves. These trends are already detectable over the historic period. Hence, it is beneficial to forecast seasonal droughts well in advance so that water managers and stakeholders can prepare to mitigate deleterious impacts. We developed a new cluster-based empirical forecast method to predict precipitation anomalies in winter. This algorithm considers not only the strength but also the pattern of the precursors. We compare our algorithm with dynamic forecast models and a canonical correlation analysis-based prediction method demonstrating that our prediction method performs better in terms of time and pattern correlation in the Mediterranean and European regions. KW - precipitation anomaly KW - seasonal forecast KW - cluster analysis Y1 - 2018 U6 - https://doi.org/10.1002/2017GL075674 SN - 0094-8276 SN - 1944-8007 VL - 44 SP - 12418 EP - 12426 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Gaedke, Ursula A1 - Klauschies, Toni T1 - Analyzing the shape of observed trait distributions enables a data-based moment closure of aggregate models JF - Limnology and Oceanography: Methods N2 - The shape of trait distributions may inform about the selective forces that structure ecological communities. Here, we present a new moment-based approach to classify the shape of observed biomass-weighted trait distributions into normal, peaked, skewed, or bimodal that facilitates spatio-temporal and cross-system comparisons. Our observed phytoplankton trait distributions exhibited substantial variance and were mostly skewed or bimodal rather than normal. Additionally, mean, variance, skewness und kurtosis were strongly correlated. This is in conflict with trait-based aggregate models that often assume normally distributed trait values and small variances. Given these discrepancies between our data and general model assumptions we used the observed trait distributions to test how well different aggregate models with first- or second-order approximations and different types of moment closure predict the biomass, mean trait, and trait variance dynamics using weakly or moderately nonlinear fitness functions. For weakly non-linear fitness functions aggregate models with a second-order approximation and a data-based moment closure that relied on the observed correlations between skewness and mean, and kurtosis and variance predicted biomass and often also mean trait changes fairly well and better than models with first-order approximations or a normal-based moment closure. In contrast, none of the models reflected the changes of the trait variances reliably. Aggregate model performance was often also poor for moderately nonlinear fitness functions. This questions a general applicability of the normal-based approach, in particular for predicting variance dynamics determining the speed of trait changes and maintenance of biodiversity. We evaluate in detail how and why better approximations can be obtained. Y1 - 2018 U6 - https://doi.org/10.1002/lom3.10218 SN - 1541-5856 VL - 15 SP - 979 EP - 994 PB - Wiley CY - Hoboken ER - TY - JOUR A1 - Kaeter, David A1 - Ziemann, Martin Andreas A1 - Böttger, Ute A1 - Weber, Iris A1 - Hecht, Lutz A1 - Voropaev, Sergey A. A1 - Korochantsev, Alexander V. A1 - Kocherov, Andrey V. T1 - The Chelyabinsk meteorite BT - new insights from a comprehensive electron microscopy and Raman spectroscopy study with evidence for graphite in olivine of ordinary chondrites JF - Meteoritics & planetary science : journal of the Meteoritical Society N2 - We present results of petrographic, mineralogical, and chemical investigations of three Chelyabinsk meteorite fragments. Three distinct lithologies were identified: light S3LL5, dark S4-S5LL5 material, and opaque fine-grained former impact melt. Olivine-spinel thermometry revealed an equilibration temperature of 703 +/- 23 degrees C for the light lithology. All plagioclase seems to be secondary, showing neither shock-induced fractures nor sulfide-metal veinlets. Feldspathic glass can be observed showing features of extensive melting and, in the dark lithology, as maskelynite, lacking melt features and retaining grain boundaries of former plagioclase. Olivine of the dark lithology shows planar deformation features. Impact melt is dominated by Mg-rich olivine and resembles whole-rock melt. Melt veins (<2mm) are connected to narrower veinlets. Melt vein textures are similar to pegmatite textures showing chilled margins, a zone of inward-grown elongated crystals and central vugs, suggesting crystallization from supercooled melt. Sulfide-metal droplets indicate liquid immiscibility of both silicate and sulfide as well as sulfide and metal melts. Impact melting may have been an important factor for differentiation of primitive planetary bodies. Graphite associated with micrometer-sized melt inclusions in primary olivine was detected by Raman mapping. Carbon isotopic studies of graphite could be applied to test a possible presolar origin. Y1 - 2017 U6 - https://doi.org/10.1111/maps.13027 SN - 1086-9379 SN - 1945-5100 VL - 53 IS - 3 SP - 416 EP - 432 PB - Wiley CY - Hoboken ER - TY - JOUR A1 - Hoffmann, Mathias A1 - Wirth, Stephan J. A1 - Bessler, Holger A1 - Engels, Christof A1 - Jochheim, Hubert A1 - Sommer, Michael A1 - Augustin, Jürgen T1 - Combining a root exclusion technique with continuous chamber and porous tube measurements for a pin-point separation of ecosystem respiration in croplands JF - Journal of plant nutrition and soil science = Zeitschrift für Pflanzenernährung und Bodenkunde N2 - To better assess ecosystem C budgets of croplands and understand their potential response to climate and management changes, detailed information on the mechanisms and environmental controls driving the individual C flux components are needed. This accounts in particular for the ecosystem respiration (R-eco) and its components, the autotrophic (R-a) and heterotrophic respiration (R-h) which vary tremendously in time and space. This study presents a method to separate R-eco into R-a [as the sum of R-a (shoot) and R-a (root)] and R-h in order to detect temporal and small-scale spatial dynamics within their relative contribution to overall R-eco. Thus, predominant environmental drivers and underlying mechanisms can be revealed. R-eco was derived during nighttime by automatic chamber CO2 flux measurements on plant covered plots. R-h was derived from CO2 efflux measurements, which were performed in parallel to R-eco measurements on a fallow plot using CO2 sampling tubes in 10 cm soil depth. R-a (root) was calculated as the difference between sampling tube CO2 efflux measurements on a plant covered plot and R-h. R-a (shoot) was calculated as R-eco - R-a (root) - R-h. Measurements were carried out for winter wheat (Triticum aestivum L.) during the crop season 2015 at an experimental plot located in the hummocky ground moraine landscape of NE Germany. R-eco varied seasonally from < 1 to 9.5 g C m(-2) d(-1), and was higher in adult (a) and reproductive (r) than juvenile (j) stands (gC m(-2) d(-1): j = 1.2, a = 4.6, r = 5.3). Observed R-a and R-h were in general smaller compared to the independently measured R-eco, contributing in average 58% and 42% to R-eco. However, both varied strongly regarding their environmental drivers and particular contribution throughout the study period, following the seasonal development of soil temperature and moisture (R-h) as well as crop development (R-a). Thus, our results consistently revealed temporal dynamics regarding the relative contribution of R-a (root) and R-a (shoot) to R-a, as well as of R-a and R-h to R-eco. Based on the observed results, implications for partitioning of R-eco in croplands are given. KW - automatic chambers KW - autotrophic respiration KW - heterotrophic respiration KW - soil CO2 sampling tubes Y1 - 2017 U6 - https://doi.org/10.1002/jpln.201600489 SN - 1436-8730 SN - 1522-2624 VL - 181 IS - 1 SP - 41 EP - 50 PB - Wiley-VCH CY - Weinheim ER - TY - JOUR A1 - Lachmuth, Susanne A1 - Henrichmann, Colette A1 - Horn, Juliane A1 - Pagel, Jörn A1 - Schurr, Frank M. T1 - Neighbourhood effects on plant reproduction BT - an experimental-analytical framework and its application to the invasive Senecio inaequidens JF - The journal of ecology N2 - Density dependence is of fundamental importance for population and range dynamics. Density-dependent reproduction of plants arises from competitive and facilitative plant-plant interactions that can be pollination independent or pollination mediated. In small and sparse populations, conspecific density dependence often turns from negative to positive and causes Allee effects. Reproduction may also increase with heterospecific density (community-level Allee effect), but the underlying mechanisms are poorly understood and the consequences for community dynamics can be complex. Allee effects have crucial consequences for the conservation of declining species, but also the dynamics of range edge populations. In invasive species, Allee effects may slow or stop range expansion. Observational studies in natural plant communities cannot distinguish whether reproduction is limited by pollination-mediated interactions among plants or by other neighbourhood effects (e.g. competition for abiotic resources). Even experimental pollen supply cannot distinguish whether variation in reproduction is caused by direct density effects or by plant traits correlated with density. Finally, it is unknown over which spatial scales pollination-mediated interactions occur. To circumvent these problems, we introduce a comprehensive experimental and analytical framework which simultaneously (1) manipulates pollen availability and quality by hand pollination and pollinator exclusion, (2) manipulates neighbourhoods by transplanting target plants, and (3) analyses the effects of con- and heterospecific neighbourhoods on reproduction with spatially explicit trait-based neighbourhood models. Synthesis. By manipulating both pollen availability and target plant locations within neighbourhoods, we can comprehensively analyse spatially explicit density dependence of plant reproduction. This experimental approach enhances our ability to understand the dynamics of sparse populations and of species geographical ranges. KW - Allee effect KW - biological invasion KW - competition KW - density dependence KW - facilitation KW - plant-plant interactions KW - pollination KW - reproductive success KW - spatially explicit model KW - trait-based neighbourhood model Y1 - 2017 U6 - https://doi.org/10.1111/1365-2745.12816 SN - 0022-0477 SN - 1365-2745 VL - 106 IS - 2 SP - 761 EP - 773 PB - Wiley CY - Hoboken ER - TY - JOUR A1 - Carus, Jana A1 - Heuner, Maike A1 - Paul, Maike A1 - Schröder, Boris T1 - Plant distribution and stand characteristics in brackish marshes BT - Unravelling the roles of abiotic factors and interspecific competition JF - Estuarine, Coastal and Shelf Science N2 - Due to increasing pressure on estuarine marshes from sea level rise and river training, there is a growing need to understand how species-environment relationships influence the zonation and growth of tidal marsh vegetation. In the present study, we investigated the distribution and stand characteristics of the two key brackish marsh species Bolboschoenus maritimus and Phragmites australis in the Elbe estuary together with several abiotic habitat factors. We then tested the effect of these habitat factors on plant growth and zonation with generalised linear models (GLMs). Our study provides detailed information on the importance of single habitat factors and their interactions for controlling the distribution patterns and stand characteristics of two key marsh species. Our results suggest that flow velocity is the main factor influencing species distribution and stand characteristics and together with soil-water salinity even affects the inundation tolerance of the two specie investigated here. Additionally, inundation height and duration as well as interspecific competition helped explain the distribution patterns and stand characteristics. By identifying the drivers of marsh zonation and stand characteristics and quantifying their effects, this study provides useful information for evaluating a future contribution of tidal marsh vegetation to ecosystem-based shore protection. KW - Bolboschoenus maritimus KW - Elbe estuary KW - Flow velocity KW - Inundation KW - Phragmites australis KW - Soil-water salinity Y1 - 2017 U6 - https://doi.org/10.1016/j.ecss.2017.06.038 SN - 0272-7714 SN - 1096-0015 VL - 196 SP - 237 EP - 247 PB - Elsevier CY - London ER - TY - JOUR A1 - Dorani, Maryam A1 - Arvin, Mohsen A1 - Oberhänsli, Roland A1 - Dargahi, Sara T1 - P-T evolution of metapelites from the Bajgan complex in the Makran accretionary prism, south eastern Iran JF - Chemie der Erde : interdisciplinary journal for chemical problems of the geo-sciences and geo-ecology = Geochemistry N2 - The Bajgan Complex, one of the basement constituents of the arc massif in Iranian Makran forms a rugged, deeply incised terrain. The complex consists of pelitic schists with minor psammitic and basic schists, calc silicate rocks, amphibolites, marbles, metavolcanosediments, mafic and felsic intrusives as well as ultramafic rocks. Metapelitic rocks show an amphibolite facies regional metamorphism and contain garnet, biotite, white mica, quartz, albite ± rutile ± apatite. Thermobarometry of garnet schist yields pressure of more than 9 kbar and temperatures between 560 and 675 °C. The geothermal gradient obtained for the peak of regional metamorphism is 19 °C/km, corresponding to a depth of ca. 31 km. Replacement of garnet by chlorite and epidote suggest greenschist facies metamorphism due to a decrease in temperature and pressure through exhumation and retrograde metamorphism (370–450 °C and 3–6 kbar). The metapelitic rocks followed a ‘clockwise’ P–T path during metamorphism, consistent with thermal decline following tectonic thickening. The formation of medium-pressure metamorphic rocks is related to presence of active subduction of the Neotethys Oceanic lithosphere beneath Eurasia in the Makran. KW - Bajgan Complex KW - Makran KW - Metapelitic rock KW - Garnet schist KW - Thermobarometry KW - Clockwise P-T path Y1 - 2017 U6 - https://doi.org/10.1016/j.chemer.2017.07.004 SN - 0009-2819 SN - 1611-5864 VL - 77 IS - 3 SP - 459 EP - 475 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Arrowsmith, J. Ramon A1 - Crosby, Christopher J. A1 - Korzhenkov, Andrey M. A1 - Mamyrov, Ernest A1 - Povolotskaya, Irina A1 - Guralnik, Benny A1 - Landgraf, Angela T1 - Surface rupture of the 1911 Kebin (Chon-Kemin) earthquake, Northern Tien Shan, Kyrgyzstan JF - Seismicity, fault rupture and earthquake hazards in slowly deforming regions N2 - The 1911 Chon-Kemin (Kebin) earthquake culminated c. 30 years of remarkable earthquakes in the northern Tien Shan (Kyrgyzstan and Kazakhstan). Building on prior mapping of the event, we traced its rupture in the field and measured more than 50 offset landforms. Cumulative fault rupture length is >155-195 km along 13 fault patches comprising six sections. The patches are separated by changes of dip magnitude or dip direction, or by 4-10 km-wide stepovers. One <40 km section overlaps and is parallel to the main north-dipping rupture but is 7 km north and dips opposite (south). Both ends of the rupture are along mountain front thrust faults demonstrating late Quaternary activity. We computed the moment from each fault patch using the surface fault traces, dip inferred from the traces, 20 km seismogenic thickness, rigidity of 3.3 x 10(10) N m(-2) and dip slip converted from our observations of the largely reverse sense of motion vertical offsets. The discontinuous patches with c. 3-4 m average slip and peak slip of <14 m yield a seismic moment of 4.6 x 10(20) Nm (M-w 7.78) to 7.4 x 10(20) Nm (M-w 7.91). The majority of moment was released along the inner eastern rupture segments. This geological moment is lower by a factor of 1.5 from that determined from teleseismic data. Y1 - 2016 SN - 978-1-86239-745-3 SN - 978-1-86239-964-8 U6 - https://doi.org/10.1144/SP432.10 SN - 0305-8719 VL - 432 SP - 233 EP - 253 PB - The Geological Society CY - London ER - TY - JOUR A1 - Landgraf, Angela A1 - Kübler, Simon A1 - Hintersberger, Esther A1 - Stein, Seth T1 - Active tectonics, earthquakes and palaeoseismicity in slowly deforming continents JF - Seismicity, fault rupture and earthquake hazards in slowly deforming regions Y1 - 2016 SN - 978-1-86239-745-3 SN - 978-1-86239-964-8 U6 - https://doi.org/10.1144/SP432.13 SN - 0305-8719 VL - 432 IS - 1 SP - 1 EP - 12 PB - The Geological Society CY - London ER - TY - JOUR A1 - Oguntunde, Philip G. A1 - Abiodun, Babatunde Joseph A1 - Lischeid, Gunnar T1 - Impacts of climate change on hydro-meteorological drought over the Volta Basin, West Africa JF - Global and planetary change N2 - This study examines the characteristics of drought in the Volta River Basin (VRB), investigates the influence of drought on the streamflow, and projects the impacts of future climate change on the drought. A combination of observation data and regional climate simulations of past and future climates (1970-2013, 2046-2065, and 2081-2100) were analyzed for the study. The Standardized Precipitation Index (SPI) and Standardized Precipitation and Evapotranspiration (SPEI) were used to characterize drought while the Standardized Runoff Index (SRI) were used to quantify runoff. Results of the study show that the historical pattern of drought is generally consistent with previous studies over the Basin and most part of West Africa. RCA ensemble medians (RMED) give realistic simulations of drought characteristics and area extent over the Basin and the sub-catchments in the past climate. Generally, an increase in drought intensity and spatial extent are projected over VRB for SPEI and SPI, but the magnitude of increase is higher with SPEI than with SPI. Drought frequency (events per decade) may be magnified by a factor of 1.2, (2046-2065) to 1.6 (2081-2100) compared to the present day episodes in the basin. The coupling between streamflow and drought episodes was very strong (P < 0.05) for the 1-16-year band before the 1970 but showed strong correlation all through the time series period for the 4-8 -years band. Runoff was highly sensitive to precipitation in the VRB and a 2-3 month time lag was found between drought indices and streamflow in the Volta River Basin. Results of this study may guide policymakers in planning how to minimize the negative impacts of future climate change that could have consequences on agriculture, water resources and energy supply. KW - Drought indices KW - Water management KW - Climate change KW - Streamfiow KW - Volta Basin Y1 - 2017 U6 - https://doi.org/10.1016/j.gloplacha.2017.07.003 SN - 0921-8181 SN - 1872-6364 VL - 155 SP - 121 EP - 132 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Baes, Marzieh A1 - Sobolev, Stephan Vladimir T1 - Mantle Flow as a Trigger for Subduction Initiation: A Missing Element of the Wilson Cycle Concept JF - Geochemistry, geophysics, geosystems N2 - The classical Wilson Cycle concept, describing repeated opening and closing of ocean basins, hypothesizes spontaneous conversion of passive continental margins into subduction zones. This process, however, is impeded by the high strength of passive margins, and it has never occurred in Cenozoic times. Here using thermomechanical models, we show that additional forcing, provided by mantle flow, which is induced by neighboring subduction zones and midmantle slab remnants, can convert a passive margin into a subduction zone. Models suggest that this is a long-term process, thus explaining the lack of Cenozoic examples. We speculate that new subduction zones may form in the next few tens of millions of years along the Argentine passive margin and the U.S. East Coast. Mantle suction force can similarly trigger subduction initiation along large oceanic fracture zones. We propose that new subduction zones will preferentially originate where subduction zones were active in the past, thus explaining the remarkable colocation of subduction zones during at least the last 400 Myr. Y1 - 2017 U6 - https://doi.org/10.1002/2017GC006962 SN - 1525-2027 VL - 18 SP - 4469 EP - 4486 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Mesbahi, Fatemeh A1 - Mohajjel, Mohammad A1 - Oberhänsli, Roland A1 - Moazzen, Mohsen T1 - The mafic rocks along the North Tabriz Fault, possible remnants of Neo-Tethys oceanic crust in NW Iran JF - Geopersia N2 - The North Tabriz Fault is seismologically an active fault with current right lateral strike-slip movements. Restricted mafic to intermediate Fate Cretaceous igneous rocks are exposed along the North Tabriz Fault. Whole rock and clinopyroxene phenocrysts geochemistry were studied in order to characterize the petrogenesis of these mafic rocks and their possible relation to an oceanic crust. The results indicate a tholeiitic parental magma that formed in an evolved mid-ocean ridge tectonic setting similar to the Iceland mid-Atlantic ridge basalts. The ocean floor basalt characteristics give evidence of an oceanic crust along the North Tabriz Fault. Therefore, the trend of the North Tabriz Fault more likely marks a suture zone related to the closure of a branch of the Neo-Tethys Ocean in the NW Iran. This fault, in addition to the Caucasus and Zagros suture zones, compensates an important part of the convergence between the Arabian and Eurasian plates resulting from the Red Sea divergence. It is concluded that the North Tabriz Fault appears to be possible southeastern continuation of the North Anatolian suture zone. KW - North Tabriz Fault KW - Mafic Rocks KW - Tholeiite KW - Late Cretaceous Y1 - 2017 U6 - https://doi.org/10.22059/geope.2017.232747.648323 SN - 2228-7817 VL - 7 SP - 301 EP - 311 PB - Graduate Faculty of Environment, University of Theran CY - Tehran ER - TY - JOUR A1 - Elmas, Ali A1 - Koralay, Ersin A1 - Duru, Olgun A1 - Schmidt, Alexander T1 - Geochronology, geochemistry, and tectonic setting of the Oligocene magmatic rocks (Marmaros Magmatic Assemblage) in Gokceada Island, northwest Turkey JF - International Geology Review N2 - Through the zmir-Ankara-Erzincan and the Vardar oceans suture zones, convergence between the Eurasian and African plates played a key role in controlling Palaeogene magmatism in north-western Anatolia, northern Aegean, and eastern Balkans. LA-ICP-MS dating of U and Pb isotopes on zircon separates from the tuffs of the Harmankaya Volcanic Rocks, which are inter-fingered with the lower-middle Eocene deposits of the Gazikoy Formation to the north of the Ganos Fault and the Karaaac Formation in the Gelibolu Peninsula, yielded a late Ypresian (51Ma) age. The chemical characteristics suggest that the lavas and tuffs of the Harmankaya Volcanic Rocks are products of syn- or post-collision magmas. These volcanic rocks show also close affinities to the subduction-related magmas. In addition to the already known andesitic volcanic rocks, our field observations in Gokceada Island indicate also the existence of granitic and rhyolitic rocks (Marmaros Magmatic Assemblage). Our U-Pb zircon age data has shown that the newly discovered Marmaros granitic plutons intruded during late Oligocene (26Ma) into the deposits of the Karaaac Formation in Gokceada Island. LA-ICP-MS dating of U and Pb isotopes on zircon separates from the Marmaros rhyolitic rocks yielded a late Oligocene (26Ma) crystallization age. Geochemical characteristics indicate that the more-evolved Oligocene granitic and rhyolitic rock of the Marmaros Magmatic Assemblage possibly assimilated a greater amount of crustal material than the lower Eocene Harmankaya Volcanic Rocks. Geochemical features and age relationships suggest increasing amounts of crustal contamination and a decreasing subduction signature during the evolution of magmas in NW Turkey from the early Eocene to the Oligocene. The magmatic activity developed following the northward subduction of the zmir-Ankara-Erzincan oceanic lithosphere and the earliest Palaeocene final continental collision between the Sakarya and Anatolide-Tauride zones. KW - U-Pb geochronology KW - geochemistry KW - granitoids KW - rhyolites KW - post-collision KW - Eocene-Oligocene KW - Gokceada Island KW - Northwestern Turkey Y1 - 2016 U6 - https://doi.org/10.1080/00206814.2016.1227941 SN - 0020-6814 SN - 1938-2839 VL - 59 IS - 4 SP - 420 EP - 447 PB - Taylor & Francis Group CY - Philadelphia ER - TY - JOUR A1 - Nord, Guillaume A1 - Boudevillain, Brice A1 - Berne, Alexis A1 - Branger, Flora A1 - Braud, Isabelle A1 - Dramais, Guillaume A1 - Gerard, Simon A1 - Le Coz, Jerome A1 - Legout, Cedric A1 - Molinie, Gilles A1 - Van Baelen, Joel A1 - Vandervaere, Jean-Pierre A1 - Andrieu, Julien A1 - Aubert, Coralie A1 - Calianno, Martin A1 - Delrieu, Guy A1 - Grazioli, Jacopo A1 - Hachani, Sahar A1 - Horner, Ivan A1 - Huza, Jessica A1 - Le Boursicaud, Raphael A1 - Raupach, Timothy H. A1 - Teuling, Adriaan J. A1 - Uber, Magdalena A1 - Vincendon, Beatrice A1 - Wijbrans, Annette T1 - A high space-time resolution dataset linking meteorological forcing and hydro-sedimentary response in a mesoscale Mediterranean catchment (Auzon) of the Ardeche region, France JF - Earth System Science Data N2 - A comprehensive hydrometeorological dataset is presented spanning the period 1 January 201131 December 2014 to improve the understanding of the hydrological processes leading to flash floods and the relation between rainfall, runoff, erosion and sediment transport in a mesoscale catchment (Auzon, 116 km(2)) of the Mediterranean region. Badlands are present in the Auzon catchment and well connected to high-gradient channels of bedrock rivers which promotes the transfer of suspended solids downstream. The number of observed variables, the various sensors involved (both in situ and remote) and the space-time resolution (similar to km(2), similar to min) of this comprehensive dataset make it a unique contribution to research communities focused on hydrometeorology, surface hydrology and erosion. Given that rainfall is highly variable in space and time in this region, the observation system enables assessment of the hydrological response to rainfall fields. Indeed, (i) rainfall data are provided by rain gauges (both a research network of 21 rain gauges with a 5 min time step and an operational network of 10 rain gauges with a 5 min or 1 h time step), S-band Doppler dual-polarization radars (1 km(2), 5 min resolution), disdrometers (16 sensors working at 30 s or 1 min time step) and Micro Rain Radars (5 sensors, 100m height resolution). Additionally, during the special observation period (SOP-1) of the HyMeX (Hydrological Cycle in the Mediterranean Experiment) project, two X-band radars provided precipitation measurements at very fine spatial and temporal scales (1 ha, 5 min). (ii) Other meteorological data are taken from the operational surface weather observation stations of Meteo-France (including 2m air temperature, atmospheric pressure, 2 m relative humidity, 10m wind speed and direction, global radiation) at the hourly time resolution (six stations in the region of interest). (iii) The monitoring of surface hydrology and suspended sediment is multi-scale and based on nested catchments. Three hydrometric stations estimate water discharge at a 2-10 min time resolution. Two of these stations also measure additional physico-chemical variables (turbidity, temperature, conductivity) and water samples are collected automatically during floods, allowing further geochemical characterization of water and suspended solids. Two experimental plots monitor overland flow and erosion at 1 min time resolution on a hillslope with vineyard. A network of 11 sensors installed in the intermittent hydrographic network continuously measures water level and water temperature in headwater subcatchments (from 0.17 to 116 km(2)) at a time resolution of 2-5 min. A network of soil moisture sensors enables the continuous measurement of soil volumetric water content at 20 min time resolution at 9 sites. Additionally, concomitant observations (soil moisture measurements and stream gauging) were performed during floods between 2012 and 2014. Finally, this dataset is considered appropriate for understanding the rainfall variability in time and space at fine scales, improving areal rainfall estimations and progressing in distributed hydrological and erosion modelling. Y1 - 2017 U6 - https://doi.org/10.5194/essd-9-221-2017 SN - 1866-3508 SN - 1866-3516 VL - 9 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Ali, Saleem H. A1 - Giurco, Damien A1 - Arndt, Nicholas A1 - Nickless, Edmund A1 - Brown, Graham A1 - Demetriades, Alecos A1 - Durrheim, Ray A1 - Enriquez, Maria Amelia A1 - Kinnaird, Judith A1 - Littleboy, Anna A1 - Meinert, Lawrence D. A1 - Oberhänsli, Roland A1 - Salem, Janet A1 - Schodde, Richard A1 - Schneider, Gabi A1 - Vidal, Olivier A1 - Yakovleva, Natalia T1 - Mineral supply for sustainable development requires resource governance JF - Nature : the international weekly journal of science N2 - Successful delivery of the United Nations sustainable development goals and implementation of the Paris Agreement requires technologies that utilize a wide range of minerals in vast quantities. Metal recycling and technological change will contribute to sustaining supply, but mining must continue and grow for the foreseeable future to ensure that such minerals remain available to industry. New links are needed between existing institutional frameworks to oversee responsible sourcing of minerals, trajectories for mineral exploration, environmental practices, and consumer awareness of the effects of consumption. Here we present, through analysis of a comprehensive set of data and demand forecasts, an interdisciplinary perspective on how best to ensure ecologically viable continuity of global mineral supply over the coming decades. Y1 - 2017 U6 - https://doi.org/10.1038/nature21359 SN - 0028-0836 SN - 1476-4687 VL - 543 SP - 367 EP - 372 PB - Nature Publ. Group CY - London ER - TY - JOUR A1 - Hoffmann, Mathias A1 - Jurisch, Nicole A1 - Alba, Juana Garcia A1 - Borraz, Elisa Albiac A1 - Schmidt, Marten A1 - Huth, Vytas A1 - Rogasik, Helmut A1 - Rieckh, Helene A1 - Verch, Gernot A1 - Sommer, Michael A1 - Augustin, Jürgen T1 - Detecting small-scale spatial heterogeneity and temporal dynamics of soil organic carbon (SOC) stocks BT - a comparison between automatic chamber-derived C budgets and repeated soil inventories JF - Biogeosciences N2 - Carbon (C) sequestration in soils plays a key role in the global C cycle. It is therefore crucial to adequately monitor dynamics in soil organic carbon (Delta SOC) stocks when aiming to reveal underlying processes and potential drivers. However, small-scale spatial (10-30 m) and temporal changes in SOC stocks, particularly pronounced in arable lands, are hard to assess. The main reasons for this are limitations of the well-established methods. On the one hand, repeated soil inventories, often used in long-term field trials, reveal spatial patterns and trends in Delta SOC but require a longer observation period and a sufficient number of repetitions. On the other hand, eddy covariance measurements of C fluxes towards a complete C budget of the soil-plant-atmosphere system may help to obtain temporal Delta SOC patterns but lack small-scale spatial resolution. To overcome these limitations, this study presents a reliable method to detect both short-term temporal dynamics as well as small-scale spatial differences of Delta SOC using measurements of the net ecosystem carbon balance (NECB) as a proxy. To estimate the NECB, a combination of automatic chamber (AC) measurements of CO2 exchange and empirically modeled aboveground biomass development (NPPshoot / were used. To verify our method, results were compared with Delta SOC observed by soil resampling. Soil resampling and AC measurements were performed from 2010 to 2014 at a colluvial depression located in the hummocky ground moraine landscape of northeastern Germany. The measurement site is characterized by a variable groundwater level (GWL) and pronounced small-scale spatial heterogeneity regarding SOC and nitrogen (Nt) stocks. Tendencies and magnitude of Delta SOC values derived by AC measurements and repeated soil inventories corresponded well. The period of maximum plant growth was identified as being most important for the development of spatial differences in annual Delta SOC. Hence, we were able to confirm that AC-based C budgets are able to reveal small-scale spatial differences and short-term temporal dynamics of Delta SOC. Y1 - 2017 U6 - https://doi.org/10.5194/bg-14-1003-2017 SN - 1726-4170 SN - 1726-4189 VL - 14 IS - 4 SP - 1003 EP - 1019 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Sirbescu, Mona-Liza C. A1 - Schmidt, Christian A1 - Veksler, Ilya V. A1 - Whittington, Alan G. A1 - Wilke, Max T1 - Experimental crystallization of undercooled felsic liquids BT - generation of pegmatitic texture JF - Journal of petrology N2 - The crystallization kinetics of silicate liquids were studied experimentally in the system haplogranite-B-Li-H2O, at variable degrees of undercooling and variable water concentration. We investigated the kinetics of nucleation and crystallization of unseeded synthetic hydrous haplogranite with 1 wt % Li2O + 2 center dot 3 wt % B2O3 added (composition C1) and 2 wt % Li2O + 4 center dot 6 wt % B2O3 added (composition C2). Compositions C1 and C2 are simplified representative bulk compositions of Li-rich pegmatites and their highly differentiated cores, respectively. Starting water contents varied between 3 and 9 wt %. With few exceptions, the system remained water-undersaturated. About 86 isothermal runs of 1-60 days duration, grouped in 25 time series of constant temperature and initial H2O content, were carried out at temperatures from 400 to 700A degrees C at 300 MPa, corresponding to variable degrees of undercooling between the liquidus and glass transition. Viscosity measurements indicate that the glass transition for both compositions is below 400A degrees C for 3 wt % water and below 300A degrees C for 6 center dot 5 wt % water. The melts remained virtually crystal free at 400A degrees C, about 100A degrees C and 120A degrees C above the glass transition for compositions C1 and C2, respectively, in experiments up to 30 days long. This result is consistent with the existence of low-temperature, undercooled melts in the crust. At lower values of undercooling the runs crystallized partially, up to about 70% volume fraction. Undercooling and the amount of water are the main factors controlling nucleation and growth rates, and therefore textures. Minerals nucleate and grow sequentially according to mineral-specific nucleation delays. The mineral assemblage started with Li-Al stuffed quartz (in C1) and virgilite (in C2), solid-solutions between quartz and gamma-spodumene. The quartz-like phases were typically followed by spherulitic alkali feldspar-quartz intergrowths, euhedral petalite, and fine-grained muscovite. Nearly pure quartz formed as rims and replacement of metastable virgilite and stuffed quartz, in particular at the boron- and water-rich crystallization front of large feldspar or petalite. With the exception of muscovite, all minerals nucleated heterogeneously, on the capsule wall or on pre-existing minerals, and grew inwards, towards the capsule center. Experimental textures resembled the textures of zoned pegmatites, including skeletal, graphic, unidirectional, radiating, spherulitic, massive, and replacement textures. In some cases, when fluid saturation was reached, miarolitic cavities developed containing euhedral crystals. Although unidirectional growth rates appeared to slow down in time, volumetric rates for stable graphic alkali-feldspar quartz intergrowths and petalite remained constant for up to 60 days and similar to 70% crystallization. Metastable stuffed quartz and virgilite diminished in their growth rates in runs of 30 days or longer, were resorbed in the melt, and were partially replaced by second-generation quartz. Unobstructed, self-sustained crystal growth in conditions of very low nucleation density appears to be the dominant mechanism to form giant pegmatitic crystals, although experimental growth rates are much slower than predicted in nature based on conductive-cooling models. KW - experimental petrology KW - lithium pegmatites KW - igneous texture KW - viscosity KW - crystal nucleation KW - crystal growth rate Y1 - 2017 U6 - https://doi.org/10.1093/petrology/egx027 SN - 0022-3530 SN - 1460-2415 VL - 58 IS - 3 SP - 539 EP - 568 PB - Oxford Univ. Press CY - Oxford ER - TY - JOUR A1 - Siddiqui, Tarique Adnan A1 - Stolle, Claudia A1 - Lühr, Hermann T1 - Longitude-dependent lunar tidal modulation of the equatorial electrojet during stratospheric sudden warmings JF - Journal of geophysical research : Space physics N2 - The effects of coupling between different layers of the atmosphere during Stratospheric Sudden Warming (SSW) events have been studied quite extensively in the past fewyears, and in this context large lunitidal enhancements in the equatorial ionosphere have also been widely discussed. In this study we report about the longitudinal variabilities in lunitidal enhancement in the equatorial electrojet (EEJ) during SSWs through ground and space observations in the Peruvian and Indian sectors. We observe that the amplification of lunitidal oscillations in EEJ is significantly larger over the Peruvian sector in comparison to the Indian sector. We further compare the lunitidal oscillations in both the sectors during the 2005-2006 and 2008-2009 major SSW events and during a non-SSW winter of 2006-2007. It is found that the lunitidal amplitude in EEJ over the Peruvian sector showed similar enhancements during both the major SSWs, but the enhancements were notably different in the Indian sector. Independent from SSW events, we have also performed a climatological analysis of the lunar modulation of the EEJ during December solstice over both the sectors by using 10years of CHAMP magnetic measurements and found larger lunitidal amplitudes over the Peruvian sector confirming the results from ground magnetometer observations. We have also analyzed the semidiurnal lunar tidal amplitude in neutral temperature measurements from Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) at 110km and found lesser longitudinal variability than the lunitidal amplitude in EEJ. Our results suggest that the longitudinal variabilities in lunitidal modulation of the EEJ during SSWs could be related to electrodynamics in the E region dynamo. KW - SSW KW - vertical coupling KW - equatorial electrojet KW - lunar tide of EEJ Y1 - 2017 U6 - https://doi.org/10.1002/2016JA023609 SN - 2169-9380 SN - 2169-9402 VL - 122 IS - 3 SP - 3760 EP - 3776 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Hoffmann, Mathias A1 - Schulz-Hanke, Maximilian A1 - Alba, Juana Garcia A1 - Jurisch, Nicole A1 - Hagemann, Ulrike A1 - Sachs, Torsten A1 - Sommer, Michael A1 - Augustin, Jürgen T1 - A simple calculation algorithm to separate high-resolution CH4 flux measurements into ebullition- and diffusion-derived components JF - Atmospheric measurement techniques : an interactive open access journal of the European Geosciences Union N2 - Processes driving the production, transformation and transport of methane (CH4 / in wetland ecosystems are highly complex. We present a simple calculation algorithm to separate open-water CH4 fluxes measured with automatic chambers into diffusion-and ebullition-derived components. This helps to reveal underlying dynamics, to identify potential environmental drivers and, thus, to calculate reliable CH4 emission estimates. The flux separation is based on identification of ebullition-related sudden concentration changes during single measurements. Therefore, a variable ebullition filter is applied, using the lower and upper quartile and the interquartile range (IQR). Automation of data processing is achieved by using an established R script, adjusted for the purpose of CH4 flux calculation. The algorithm was validated by performing a laboratory experiment and tested using flux measurement data (July to September 2013) from a former fen grassland site, which converted into a shallow lake as a result of rewetting. Ebullition and diffusion contributed equally (46 and 55 %) to total CH4 emissions, which is comparable to ratios given in the literature. Moreover, the separation algorithm revealed a concealed shift in the diurnal trend of diffusive fluxes throughout the measurement period. The water temperature gradient was identified as one of the major drivers of diffusive CH4 emissions, whereas no significant driver was found in the case of erratic CH4 ebullition events. Y1 - 2017 U6 - https://doi.org/10.5194/amt-10-109-2017 SN - 1867-1381 SN - 1867-8548 VL - 10 IS - 1 SP - 109 EP - 118 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Molnos, Sonja A1 - Mamdouh, Tarek A1 - Petri, Stefan A1 - Nocke, Thomas A1 - Weinkauf, Tino A1 - Coumou, Dim T1 - A network-based detection scheme for the jet stream core JF - Earth system dynamics N2 - The polar and subtropical jet streams are strong upper-level winds with a crucial influence on weather throughout the Northern Hemisphere midlatitudes. In particular, the polar jet is located between cold arctic air to the north and warmer subtropical air to the south. Strongly meandering states therefore often lead to extreme surface weather. The parameter values of the detection scheme are optimized using simulated annealing and a skill function that accounts for the zonal-mean jet stream position (Rikus, 2015). After the successful optimization process, we apply our scheme to reanalysis data covering 1979-2015 and calculate seasonal-mean probabilistic maps and trends in wind strength and position of jet streams. We present longitudinally defined probability distributions of the positions for both jets for all on the Northern Hemisphere seasons. This shows that winter is characterized by two well-separated jets over Europe and Asia (ca. 20 degrees W to 140 degrees E). In contrast, summer normally has a single merged jet over the western hemisphere but can have both merged and separated jet states in the eastern hemisphere. Y1 - 2017 U6 - https://doi.org/10.5194/esd-8-75-2017 SN - 2190-4979 SN - 2190-4987 VL - 8 IS - 1 SP - 75 EP - 89 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Loritz, Ralf A1 - Hassler, Sibylle K. A1 - Jackisch, Conrad A1 - Allroggen, Niklas A1 - van Schaik, Loes A1 - Wienhöfer, Jan A1 - Zehe, Erwin T1 - Picturing and modeling catchments by representative hillslopes JF - Hydrology and earth system sciences : HESS N2 - This study explores the suitability of a single hillslope as a parsimonious representation of a catchment in a physically based model. We test this hypothesis by picturing two distinctly different catchments in perceptual models and translating these pictures into parametric setups of 2-D physically based hillslope models. The model parametrizations are based on a comprehensive field data set, expert knowledge and process-based reasoning. Evaluation against streamflow data highlights that both models predicted the annual pattern of streamflow generation as well as the hydrographs acceptably. However, a look beyond performance measures revealed deficiencies in streamflow simulations during the summer season and during individual rainfall-runoff events as well as a mismatch between observed and simulated soil water dynamics. Some of these shortcomings can be related to our perception of the systems and to the chosen hydrological model, while others point to limitations of the representative hillslope concept itself. Nevertheless, our results confirm that representative hillslope models are a suitable tool to assess the importance of different data sources as well as to challenge our perception of the dominant hydrological processes we want to represent therein. Consequently, these models are a promising step forward in the search for the optimal representation of catchments in physically based models. Y1 - 2017 U6 - https://doi.org/10.5194/hess-21-1225-2017 SN - 1027-5606 SN - 1607-7938 VL - 21 IS - 2 SP - 1225 EP - 1249 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Barthold, Frauke Katrin A1 - Turner, Benjamin L. A1 - Elsenbeer, Helmut A1 - Zimmermann, Alexander T1 - A hydrochemical approach to quantify the role of return flow in a surface flow-dominated catchment JF - Hydrological processes N2 - Stormflow generation in headwater catchments dominated by subsurface flow has been studied extensively, yet catchments dominated by surface flow have received less attention. We addressed this by testing whether stormflow chemistry is controlled by either (a) the event-water signature of overland flow, or (b) the pre-event water signature of return flow. We used a high-resolution hydrochemical data set of stormflow and end-members of multiple storms in an end-member mixing analysis to determine the number of end-members needed to explain stormflow, characterize and identify potential end-members, calculate their contributions to stormflow, and develop a conceptual model of stormflow. The arrangement and relative positioning of end-members in stormflow mixing space suggest that saturation excess overland flow (26-48%) and return flow from two different subsurface storage pools (17-53%) are both similarly important for stormflow. These results suggest that pipes and fractures are important flow paths to rapidly release stored water and highlight the value of within-event resolution hydrochemical data to assess the full range and dynamics of flow paths. KW - EMMA KW - hydrochemistry KW - overland flow KW - return flow KW - stormflow generation Y1 - 2016 U6 - https://doi.org/10.1002/hyp.11083 SN - 0885-6087 SN - 1099-1085 VL - 31 IS - 5 SP - 1018 EP - 1033 PB - Wiley CY - Hoboken ER - TY - JOUR A1 - Li, Shaoyang A1 - Moreno Switt, Marcos A1 - Bedford, Jonathan A1 - Rosenau, Matthias A1 - Heidbach, Oliver A1 - Melnick, Daniel A1 - Oncken, Onno T1 - Postseismic uplift of the Andes following the 2010 Maule earthquake BT - Implications for mantle rheology JF - Geophysical research letters N2 - Postseismic surface deformation associated with great subduction earthquakes is controlled by asthenosphere rheology, frictional properties of the fault, and structural complexity. Here by modeling GPS displacements in the 6 years following the 2010 M-w 8.8 Maule earthquake in Chile, we investigate the impact of heterogeneous viscosity distribution in the South American subcontinental asthenosphere on the 3-D postseismic deformation pattern. The observed postseismic deformation is characterized by flexure of the South America plate with peak uplift in the Andean mountain range and subsidence in the hinterland. We find that, at the time scale of observation, over 2 orders of magnitude gradual increase in asthenosphere viscosity from the arc area toward the cratonic hinterland is needed to jointly explain horizontal and vertical displacements. Our findings present an efficient method to estimate spatial variations of viscosity, which clearly improves the fitting to the vertical signal of deformation. Lateral changes in asthenosphere viscosity can be correlated with the thermomechanical transition from weak subvolcanic arc mantle to strong subcratonic mantle, thus suggesting a stationary heterogeneous viscosity structure. However, we cannot rule out a transient viscosity structure (e.g., power law rheology) with the short time span of observation. Y1 - 2017 U6 - https://doi.org/10.1002/2016GL071995 SN - 0094-8276 SN - 1944-8007 VL - 44 IS - 4 SP - 1768 EP - 1776 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Campforts, Benjamin A1 - Schwanghart, Wolfgang A1 - Govers, Gerard T1 - Accurate simulation of transient landscape evolution by eliminating numerical diffusion BT - the TTLEM 1.0 model JF - Earth surface dynamics N2 - Landscape evolution models (LEMs) allow the study of earth surface responses to changing climatic and tectonic forcings. While much effort has been devoted to the development of LEMs that simulate a wide range of processes, the numerical accuracy of these models has received less attention. Most LEMs use first-order accurate numerical methods that suffer from substantial numerical diffusion. Numerical diffusion particularly affects the solution of the advection equation and thus the simulation of retreating landforms such as cliffs and river knickpoints. This has potential consequences for the integrated response of the simulated landscape. Here we test a higher-order flux-limiting finite volume method that is total variation diminishing (TVD-FVM) to solve the partial differential equations of river incision and tectonic displacement. We show that using the TVD-FVM to simulate river incision significantly influences the evolution of simulated landscapes and the spatial and temporal variability of catchment-wide erosion rates. Furthermore, a two-dimensional TVD-FVM accurately simulates the evolution of landscapes affected by lateral tectonic displacement, a process whose simulation was hitherto largely limited to LEMs with flexible spatial discretization. We implement the scheme in TTLEM (TopoToolbox Landscape Evolution Model), a spatially explicit, raster-based LEM for the study of fluvially eroding landscapes in TopoToolbox 2. Y1 - 2017 U6 - https://doi.org/10.5194/esurf-5-47-2017 SN - 2196-6311 SN - 2196-632X VL - 5 IS - 1 SP - 47 EP - 66 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Endepols, Stefan A1 - Klemann, Nicole A1 - Richter, Dania A1 - Matuschka, Franz-Rainer T1 - The potential of coumatetralyl enhanced by cholecalciferol in the control of anticoagulant-resistant Norway rats (Rattus norvegicus) JF - Pest management science N2 - BACKGROUND: We evaluated the potential of cholecalciferol as an enhancer of the first-generation anticoagulant coumatetralyl in the Westphalia anticoagulant-resistant strain of the Norway rat (Rattus norvegicus Berkenhout), characterised by the Tyr139Cys polymorphism on the VKOR enzyme. Because today only the most potent, but also most persistent anticoagulant rodenticides of the second generation remain available to control this strain, new rodenticide solutions are required. RESULTS: Feeding trials in the laboratory confirmed a significant level of efficacy, which was corroborated by field trials in the Munsterland resistance area. After frequency and level of resistance were assessed by blood clotting response tests, field trials were conducted with bait containing coumatetralyl at 375 mg kg(-1) and cholecalciferol at 50 mg kg(-1) or 100 mg kg(-1). Control success was 94% when a large rat infestation comprising 42% resistant animals was treated. Another field trial applying the combination to a rat population that had survived a preceding treatment with bromadiolone resulted in a 99.5% control success according to the first census day, but with some increase in rat activity during subsequent census days. CONCLUSION: The combination of coumatetralyl and cholecalciferol is a promising alternative approach to the most potent second-generation anticoagulants in resistance management, particularly in respect of environmental risks, such as secondary poisoning. (C) 2016 Society of Chemical Industry KW - rodent control KW - Norway rat KW - Rattus norvegicus KW - resistance KW - cholecalciferol KW - coumatetralyl Y1 - 2017 U6 - https://doi.org/10.1002/ps.4235 SN - 1526-498X SN - 1526-4998 VL - 73 IS - 2 SP - 280 EP - 286 PB - Wiley CY - Hoboken ER - TY - JOUR A1 - Hand, Ralf A1 - Grossmann, Anita A1 - Lauterbach, Daniel T1 - Endemics and their common congener plant species on an East Mediterranean island BT - a comparative functional trait approach JF - Plant ecology : an international journal N2 - Understanding evolution and ecology of endemic plants is of great importance for conservation of those rare and endangered species. Pairwise comparisons of plant functional traits could be an adequate method to get insights in evolutionary and ecological processes. We examined whether morphological traits representing competitive ability and habitat specificity differ between endemics and common plants. Therefore, we performed pairwise comparison analyses of 9 plant functional traits in 36 congeneric pairs of endemics and their common congeners on the East Mediterranean island of Cyprus, i.e., the first such study conducted on a Mediterranean island. We found that endemic species prefer higher elevations and more extreme habitats. Endemics were smaller and they had smaller flowers than their common congeners. Common species had higher chromosome numbers than endemic ones. Endemic and common species showed no significant differences in canopy height, inflorescence height, leaf length and width, and flowering period. Our study showed that the situation on a large oceanic island does not differ from results in mainland research areas. KW - Biodiversity hotspot KW - Mediterranean Basin KW - Cyprus KW - Endemism KW - Rare common comparison Y1 - 2017 U6 - https://doi.org/10.1007/s11258-016-0673-y SN - 1385-0237 SN - 1573-5052 VL - 218 SP - 139 EP - 150 PB - Springer CY - Dordrecht ER - TY - JOUR A1 - Ghasemizade, Mehdi A1 - Baroni, Gabriele A1 - Abbaspour, Karim A1 - Schirmer, Mario T1 - Combined analysis of time-varying sensitivity and identifiability indices to diagnose the response of a complex environmental model JF - Environmental modelling & software with environment data news N2 - Sensitivity and identifiability analyses are common diagnostic tools to address over-parametrization in complex environmental models, but a combined application of the two analyses is rarely conducted. In this study, we performed a temporal global sensitivity analysis using the variance-based method of Sobol’ and a temporal identifiability analysis of model parameters using the dynamic identifiability method (DYNIA). We discuss the relationship between the two analyses with a focus on parameter identification and output uncertainty reduction. The hydrological model HydroGeoSphere was used to simulate daily evapotranspiration, water content, and seepage at the lysimeter scale. We found that identifiability of a parameter does not necessarily reduce output uncertainty. It was also found that the information from the main and total effects (main Sobol' sensitivity indices) is required to allow uncertainty reduction in the model output. Overall, the study highlights the role of combined temporal diagnostic tools for improving our understanding of model behavior. KW - Temporal sensitivity KW - Identifiability KW - Preferential flow KW - HydroGeoSphere KW - Output uncertainty Y1 - 2016 U6 - https://doi.org/10.1016/j.envsoft.2016.10.011 SN - 1364-8152 SN - 1873-6726 VL - 88 SP - 22 EP - 34 PB - Elsevier CY - Oxford ER - TY - JOUR A1 - Nelson, Daniel B. A1 - Knohl, Alexander A1 - Sachse, Dirk A1 - Schefulss, Enno A1 - Kahmen, Ansgar T1 - Sources and abundances of leaf waxes in aerosols in central Europe JF - Geochimica et cosmochimica acta : journal of the Geochemical Society and the Meteoritical Society N2 - Atmospheric transport is an understudied mechanism for leaf wax hydrogen isotope applications that contributes to mobilizing and depositing these compounds on the surface of the Earth. While previous efforts have identified the importance of atmospheric leaf wax deposition in remote marine locations, the processes are not well constrained on land in temperate latitudes where lakes are common and sedimentary leaf wax hydrogen isotope values are an attractive tool for understanding past precipitation changes. This work presents results from a field study that was conducted in 2010 and 2011 at Hainich National Park, Germany in order to evaluate the quantity and sources of leaf waxes in the atmosphere. Aerosols were sampled at approximately weekly intervals inside the forest canopy, and n-alkane distributions and hydrogen isotope values were compared with those from major tree species surrounding the sampling site. Despite sampling in what was expected to be a major production center, the distribution and hydrogen isotope values of atmospheric n-alkanes bore little resemblance to those of the local vegetation. Comparison with local meteorological data and to 10-day and 36-h back air mass trajectories indicated shifting effects of winds and temperature, and that mesoscale transport processes were more important than longrange mechanisms. Back trajectories also highlighted source effects, with easterly winds coinciding with relatively lower leaf wax hydrogen isotope values from more continental regions. These results suggest that leaf wax aerosols average over spatial scales that exceed typical surface catchment areas for small lake systems, even in forested areas, yet that the area over which these compounds are derived is still relatively regional. Depositional fluxes were also estimated in order to assess the potential importance of atmospheric transport to sedimentary archives. Although difficult to constrain, these estimates suggest that atmospheric deposition may be non-negligible for lake systems in cases where inputs from rivers or surface runoff are limited. Together, these observations provide new insights on how leaf waxes from different sources are integrated during aeolian transport and the spatial scales over which these processes occur. KW - Hydrogen isotopes KW - Leaf wax KW - Aerosols KW - n-Alkanes KW - Biomarkers KW - Lakes KW - Sediments Y1 - 2016 U6 - https://doi.org/10.1016/j.gca.2016.11.018 SN - 0016-7037 SN - 1872-9533 VL - 198 SP - 299 EP - 314 PB - Elsevier CY - Oxford ER - TY - JOUR A1 - Melnick, Daniel A1 - Moreno, Marcos A1 - Quinteros, Javier A1 - Carlos Baez, Juan A1 - Deng, Zhiguo A1 - Li, Shaoyang A1 - Oncken, Onno T1 - The super-interseismic phase of the megathrust earthquake cycle in Chile JF - Geophysical research letters N2 - Along a subduction zone, great megathrust earthquakes recur either after long seismic gaps lasting several decades to centuries or over much shorter periods lasting hours to a few years when cascading successions of earthquakes rupture nearby segments of the fault. We analyze a decade of continuous Global Positioning System observations along the South American continent to estimate changes in deformation rates between the 2010 Maule (M8.8) and 2015 Illapel (M8.3) Chilean earthquakes. We find that surface velocities increased after the 2010 earthquake, in response to continental-scale viscoelastic mantle relaxation and to regional-scale increased degree of interplate locking. We propose that increased locking occurs transiently during a super-interseismic phase in segments adjacent to a megathrust rupture, responding to bending of both plates caused by coseismic slip and subsequent afterslip. Enhanced strain rates during a super-interseismic phase may therefore bring a megathrust segment closer to failure and possibly triggered the 2015 event. KW - megathrust KW - earthquake KW - cycle KW - Chile Y1 - 2017 U6 - https://doi.org/10.1002/2016GL071845 SN - 0094-8276 SN - 1944-8007 VL - 44 IS - 2 SP - 784 EP - 791 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Kozicka, Marta A1 - Kalkuhl, Matthias A1 - Brockhaus, Jan T1 - Food Grain Policies in India and their Implications for Stocks and Fiscal Costs BT - a Dynamic Partial Equilibrium Analysis JF - Journal of Agricultural Economics N2 - We analyse current and possible future reforms of the Indian food policies for the most important staple grains, wheat and rice, within a two-commodity dynamic partial equilibrium model with stochastic shocks. The model is empirically grounded and reproduces past values well. It uses a new reduced-form approach to capture private storage dynamics. We evaluate the implementation of the National Food Security Act (NFSA) under several policy measures with the current regime as well as two scenarios with a regime change - implementation of cash transfers and deficiency payments. Implications for market fundamentals and fiscal costs are simulated in the medium term - until 2020/21. The NFSA puts a high pressure on fiscal costs and public stocks. Relying on imports with low support prices results in low fiscal costs and stable, but higher domestic and international prices, and a high risk of zero stocks. A policy strategy to manipulate procurement prices in order to maintain public stocks close to the norms leads to slightly higher fiscal costs with lower, but more volatile prices. The highest domestic price volatility occurs under a strategy which uses export bans in order to maintain sufficient public stocks. A cash-based regime can bring considerable savings and curb fiscal costs, particularly if targeted to the poor, and would leave sufficient stocks due to higher private stocks. KW - Fiscal costs KW - food grain policies KW - grain storage KW - India KW - NFSA KW - reforms Y1 - 2017 U6 - https://doi.org/10.1111/1477-9552.12176 SN - 0021-857X SN - 1477-9552 VL - 68 IS - 1 SP - 98 EP - 122 PB - Wiley-Blackwell CY - Hoboken ER - TY - JOUR A1 - Jones, Benjamin M. A1 - Arp, Christopher D. A1 - Whitman, Matthew S. A1 - Nigro, Debora A1 - Nitze, Ingmar A1 - Beaver, John A1 - Gadeke, Anne A1 - Zuck, Callie A1 - Liljedahl, Anna A1 - Daanen, Ronald A1 - Torvinen, Eric A1 - Fritz, Stacey A1 - Grosse, Guido T1 - A lake-centric geospatial database to guide research and inform management decisions in an Arctic watershed in northern Alaska experiencing climate and land-use changes JF - AMBIO N2 - Lakes are dominant and diverse landscape features in the Arctic, but conventional land cover classification schemes typically map them as a single uniform class. Here, we present a detailed lake-centric geospatial database for an Arctic watershed in northern Alaska. We developed a GIS dataset consisting of 4362 lakes that provides information on lake morphometry, hydrologic connectivity, surface area dynamics, surrounding terrestrial ecotypes, and other important conditions describing Arctic lakes. Analyzing the geospatial database relative to fish and bird survey data shows relations to lake depth and hydrologic connectivity, which are being used to guide research and aid in the management of aquatic resources in the National Petroleum Reserve in Alaska. Further development of similar geospatial databases is needed to better understand and plan for the impacts of ongoing climate and land-use changes occurring across lake-rich landscapes in the Arctic. KW - Arctic KW - Climate Change KW - GIS KW - Lakes KW - Land-use change KW - Watershed Y1 - 2017 U6 - https://doi.org/10.1007/s13280-017-0915-9 SN - 0044-7447 SN - 1654-7209 VL - 46 SP - 769 EP - 786 PB - Springer CY - Dordrecht ER - TY - JOUR A1 - Lu, Honghua A1 - Cheng, Lu A1 - Wang, Zhen A1 - Zhang, Tianqi A1 - Lu, Yanwu A1 - Zhao, Junxiang A1 - Li, Youli A1 - Zheng, Xiangmin T1 - Latest Quaternary rapid river incision across an inactive fold in the northern Chinese Tian Shan foreland JF - Quaternary science reviews : the international multidisciplinary research and review journal N2 - This work focuses on the incision process over the Tuostai anticline, a fold of the proximal structure Belt I in the northern Chinese Tian Shan foreland, where the Sikeshu River has incised deeply into the alluvial gravels and the fold's underlying bedrock strata. Field investigation and geomorphic mapping define five terraces of the Sikeshu River (designated as T1 to T5 from oldest to youngest) preserved within the Tuostai anticline. 10Be surface exposure dating and optically stimulated luminescence dating constrain stabilization of the highest three terrace surfaces at about 80 ka (T1), 16 ka (T2), and 15 ka (T3), respectively. Around 16 ka, the calculated river incision rates significantly increase from <2 mm/yr to >6 mm/yr. Undeformed longitudinal profiles of terraces T2, T3 and T4 over the Tuostai anticline suggest that this structure may have been tectonically inactive since stabilization of these three terraces. We thus think that the observed rapid river incision over the Tuostai anticline has not been largely forced by tectonic uplift. Instead, the progressively warmer and wetter palaeoclimatic condition within the Tian Shan range and its surrounding area during the period of ∼20–10 ka may have enhanced river incision across the Tuostai anticline. A reduced sediment/water ratio might have lowered the gradient of the Sikeshu River. KW - River incision KW - Fluvial terrace KW - Palaeoclimate KW - Late Quaternary KW - Tian Shan Y1 - 2017 U6 - https://doi.org/10.1016/j.quascirev.2017.10.017 SN - 0277-3791 VL - 179 SP - 167 EP - 181 PB - Elsevier CY - Oxford ER - TY - JOUR A1 - Frolova, Larissa A. A1 - Ibragimova, A. G. A1 - Subetto, D. A. A1 - Nazarova, Larisa B. A1 - Syrykh, Lydmila S. T1 - Paleoecological and paleoclimatic reconstructions for the Karelian Isthmus based on the study of subfossil cladocerans from Lake Medvedevskoe (Northwest Russia) JF - Učënye Zapiski Kazanskogo Universiteta. Seriâ Estestvennye Nauki JF - Proceedings of Kazan University. Natural Sciences Series N2 - The purpose of our study is to reconstruct the climatic and environmental changes that took place over the Holocene in Northwest Russia. The results of the palaeobiological analysis of cladoceran community of Lake Medvedevskoe (Karelian Isthmus, located between the Gulf of Finland of the Baltic Sea and Lake Ladoga, Northwest Russia) have been discussed. In the sediments of Lake Medvedevskoe, we have identified 38 cladoceran taxa that belong to 7 families: Bosminidae, Holopedidae, Chydoridae, Daphnidae, Polyphemidae, Macrotricidae, and Sididae. It has been revealed that Bosmina (Eubosmina) longispina and Alonella nana are the most common for subfossil Cladocera community of the lake. Palearctic and Holarctic species are dominant. Both pelagic and littoral taxa are well represented in the lake. The down-core changes in cladoceran community allowed to identify five statistically significant zones. It has been discovered that the taxonomic richness of biological communities is low at the bottom of the core with the dominance of typical northern species and increases towards the sediment surface alongside with the rise of organic content in sediments. Based on the shifts in the taxonomic composition of cladoceran community, we have concluded upon the trophic status of the lake and climate changes. The obtained data have been compared with the results of the chironomid analysis that was performed earlier. KW - paleoclimatic reconstructions KW - subfossil Cladocera KW - Lake Medvedevskoe KW - Karelian Isthmus Y1 - 2017 SN - 2542-064X SN - 2500-218X VL - 160 IS - 1 SP - 93 EP - 110 PB - Kazan Federal University CY - Kazan ER - TY - JOUR A1 - Hoffmann, Matthias A1 - Pohl, Madlen A1 - Jurisch, N. A1 - Prescher, Anne-Katrin A1 - Campa, E. Mendez A1 - Hagemann, Ulrike A1 - Remus, R. A1 - Verch, G. A1 - Sommer, Michael A1 - Augustin, J. T1 - Maize carbon dynamics are driven by soil erosion state and plant phenology rather than nitrogen fertilization form JF - Soil & tillage research : an international journal on research and development in soil tillage and field traffic, and their relationships with soil environment, land use and crop production N2 - Carbon (C) stored in soils represents the largest C pool of terrestrial ecosystems and consequently plays a crucial role in the global C cycle. So far, it is widely unclear to what extent different land uses and land use change influence soil C storage. The hummocky ground moraine landscape of northeastern Germany is characterized by distinct small-scale soil heterogeneity on the one hand, and intensive energy crop cultivation on the other. Both factors are assumed to significantly influence gaseous C exchange; as such, they likely drive soil organic carbon (SOC) stock dynamics in terrestrial agricultural ecosystems. To date, it is not clear to what extent N fertilization forms, which are associated with energy crop cultivation (e.g., application of biogas fermentation residues) and soil type relative to soil erosion state, influence soil C dynamics, nor is it clear whether one of these factors is more important than the other. To investigate the influence of soil erosion state and N fertilization form on soil C dynamics, we present dynamic and seasonal net ecosystem carbon balances (NECB) as a proxy for changes in soil organic carbon stocks. Measurements were conducted for maize (Zea mays L.) at five sites in the "CarboZALF-D" experimental field during the 2011 growing season. Measurement sites represent different soil erosion states (non-eroded Albic Luvisols, extremely eroded Calcaric Regosols and depositional Endogleyic Colluvic Regosols) and N fertilization forms (100% mineral fertilizer, 50% mineral and 50% organic fertilizer, and 100% organic fertilizer). Fertilization treatments were established on the Albic Luvisol. Net ecosystem CO2 exchange (NEE) and ecosystem respiration (R-eco) were measured every four weeks using a dynamic flow-through non-steady-state closed manual chamber system. Gap filling was performed based on empirical temperature and PAR dependency functions and was used to derive daily NEE values. In parallel, daily above-ground biomass production (NPFshoot) was estimated using a logistic growth equation, fitted on periodic biomass samples. Finally, C dynamics were calculated as the balance of daily NEE and NPPshoot based on the initial C input due to organic fertilization. Resulting NECB varied from pronounced soil C losses at the Endogleyic Colluvic Regosol (592 g C m(-2)) to soil C gains at the Calcaric Regosol (-124 g C m(-2)). Minor to modest C losses were observed for the Albic Luvisol. Compared to N fertilization forms, soil erosion states generally had a stronger impact on derived NECB. However, interannual variations in plant phonology and interactions between soil erosion states and fertilization forms might result in different NECB values over multiple years. Hence, long-term measurements of different fertilization treatments on characteristic soil landscape elements are needed. KW - Soil erosion KW - Net ecosystem carbon balance (NECB) KW - Closed chamber measurements KW - Biogas fermentation residues KW - Plant phenology Y1 - 2017 U6 - https://doi.org/10.1016/j.still.2017.09.004 SN - 0167-1987 SN - 1879-3444 VL - 175 SP - 255 EP - 266 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Julier, Adele C. M. A1 - Jardine, Phillip E. A1 - Adu-Bredu, Stephen A1 - Coe, Angela L. A1 - Duah-Gyamfi, Akwasi A1 - Fraser, Wesley T. A1 - Lomax, Barry H. A1 - Malhi, Yadvinder A1 - Moore, Sam A1 - Owusu-Afriyie, Kennedy A1 - Gosling, William D. T1 - The modern pollen-vegetation relationships of a tropical forest-savannah mosaic landscape, Ghana, West Africa JF - Palynology N2 - Transitions between forest and savannah vegetation types in fossil pollen records are often poorly understood due to over-production by taxa such as Poaceae and a lack of modern pollen-vegetation studies. Here, modern pollen assemblages from within a forest-savannah transition in West Africa are presented and compared, their characteristic taxa discussed, and implications for the fossil record considered. Fifteen artificial pollen traps were deployed for 1 year, to collect pollen rain from three vegetation plots within the forest-savannah transition in Ghana. High percentages of Poaceae and Melastomataceae/Combretaceae were recorded in all three plots. Erythrophleum suaveolens characterised the forest plot, Manilkara obovata the transition plot and Terminalia the savannah plot. The results indicate that Poaceae pollen influx rates provide the best representation of the forest-savannah gradient, and that a Poaceae abundance of >40% should be considered as indicative of savannah-type vegetation in the fossil record. KW - pollen KW - transitions KW - Poaceae KW - savannah KW - Ghana KW - palaeoecology KW - Bosumtwi Y1 - 2017 U6 - https://doi.org/10.1080/01916122.2017.1356392 SN - 0191-6122 SN - 1558-9188 VL - 42 IS - 3 SP - 324 EP - 338 PB - Taylor & Francis Group CY - Philadelphia ER - TY - GEN A1 - Wetzel, Maria A1 - Kempka, Thomas A1 - Kühn, Michael T1 - Predicting macroscopic elastic rock properties requires detailed information on microstructure T2 - Energy procedia N2 - Predicting variations in macroscopic mechanical rock behaviour due to microstructural changes, driven by mineral precipitation and dissolution is necessary to couple chemo-mechanical processes in geological subsurface simulations. We apply 3D numerical homogenization models to estimate Young’s moduli for five synthetic microstructures, and successfully validate our results for comparable geometries with the analytical Mori-Tanaka approach. Further, we demonstrate that considering specific rock microstructures is of paramount importance, since calculated elastic properties may deviate by up to 230 % for the same mineral composition. Moreover, agreement between simulated and experimentally determined Young’s moduli is significantly improved, when detailed spatial information are employed. KW - digital rock physics KW - effective elastic properties KW - numerical Y1 - 2017 U6 - https://doi.org/10.1016/j.egypro.2017.08.195 SN - 1876-6102 VL - 125 SP - 561 EP - 570 PB - Elsevier CY - Amsterdam ER - TY - GEN A1 - Kühn, Michael A1 - Schöne, Tim T1 - Multivariate regression model from water level and production rate time series for the geothermal reservoir Waiwera (New Zealand) T2 - Energy procedia N2 - Water management tools are necessary to guarantee the preservation of natural resources while ensuring optimum utilization. Linear regression models are a simple and quick solution for creating prognostic capabilities. Multivariate models show higher precision than univariate models. In the case of Waiwera, implementation of individual production rates is more accurate than applying just the total production rate. A maximum of approximately 1,075 m3/day can be pumped to ensure a water level of at least 0.5 m a.s.l. in the monitoring well. The model should be renewed annually to implement new data and current water level trends to keep the quality. KW - geothermal reservoir KW - water management KW - data based model KW - multivariate regression KW - coefficient of determination KW - scenario analysis Y1 - 2017 U6 - https://doi.org/10.1016/j.egypro.2017.08.196 SN - 1876-6102 VL - 125 SP - 571 EP - 579 PB - Elsevier CY - Amsterdam ER - TY - GEN A1 - Kühn, Michael A1 - Li, Qi A1 - Nakaten, Natalie Christine A1 - Kempka, Thomas T1 - Integrated subsurface gas storage of CO2 and CH4 offers capacity and state-of-the-art technology for energy storage in China T2 - Energy procedia N2 - Integration and development of the energy supply in China and worldwide is a challenge for the years to come. The innovative idea presented here is based on an extension of the “power-to-gas-to-power” technology by establishing a closed carbon cycle. It is an implementation of a low-carbon energy system based on carbon dioxide capture and storage (CCS) to store and reuse wind and solar energy. The Chenjiacun storage project in China compares well with the German case study for the towns Potsdam and Brandenburg/Havel in the Federal State of Brandenburg based on the Ketzin pilot site for CCS. KW - gas storage KW - carbon dioxide KW - methane KW - hydrogen KW - renewable energy KW - carbon cycle Y1 - 2017 U6 - https://doi.org/10.1016/j.egypro.2017.08.039 SN - 1876-6102 VL - 125 SP - 14 EP - 18 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Pick, Leonie A1 - Korte, Monika T1 - An annual proxy for the geomagnetic signal of magnetospheric currents on Earth based on observatory data from 1900–2010 JF - Geophysical Journal International N2 - We introduce the Annual Magnetospheric Currents index as long-term proxy for the geomagnetic signal of magnetospheric currents on Earth valid within the time span 1900–2010. Similar to the widely used disturbance storm time and ‘Ring Current’ indices, it is based on geomagnetic observatory data, but provides a realistic absolute level and uncertainty estimates. Crucial aspects to this end are the revision of observatory crustal biases as well as the implementation of a Bayesian inversion accounting for uncertainties in the main field estimate, both required for the index derivation. The observatory choice is based on a minimization of index variance during a reference period spanning 1960–2010. The new index is capable of correcting observatory time series from large-scale external signals in a user-friendly manner. At present the index is only available as annual mean values. An extension to hourly values for the same time span is in progress. KW - Magnetic field variations through time KW - Satellite magnetics KW - Inverse theory KW - Statistical methods KW - Time-series analysis Y1 - 2017 U6 - https://doi.org/10.1093/gji/ggx367 SN - 1365-246X SN - 0956-540X VL - 211 IS - 2 SP - 1223 EP - 1236 PB - Oxford Univ. Press CY - Oxford ER - TY - GEN A1 - Milewski, Robert A1 - Chabrillat, Sabine A1 - Behling, Robert T1 - Analyses of Recent Sediment Surface Dynamic of a Namibian Kalahari Salt Pan Based on Multitemporal Landsat and Hyperspectral Hyperion Data T2 - Postprints der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe N2 - This study combines spaceborne multitemporal and hyperspectral data to analyze the spatial distribution of surface evaporite minerals and changes in a semi-arid depositional environment associated with episodic flooding events, the Omongwa salt pan (Kalahari, Namibia). The dynamic of the surface crust is evaluated by a change-detection approach using the Iterative-reweighted Multivariate Alteration Detection (IR-MAD) based on the Landsat archive imagery from 1984 to 2015. The results show that the salt pan is a highly dynamic and heterogeneous landform. A change gradient is observed from very stable pan border to a highly dynamic central pan. On the basis of hyperspectral EO-1 Hyperion images, the current distribution of surface evaporite minerals is characterized using Spectral Mixture Analysis (SMA). Assessment of field and image endmembers revealed that the pan surface can be categorized into three major crust types based on diagnostic absorption features and mineralogical ground truth data. The mineralogical crust types are related to different zones of surface change as well as pan morphology that influences brine flow during the pan inundation and desiccation cycles. These combined information are used to spatially map depositional environments where the more dynamic halite crust concentrates in lower areas although stable gypsum and calcite/sepiolite crusts appear in higher elevated areas. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 987 KW - salt pan KW - playa KW - hyperspectral KW - multitemporal KW - change detection KW - evaporite minerals Y1 - 2020 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-475642 SN - 1866-8372 IS - 987 ER - TY - THES A1 - Meier, Tobias T1 - Borehole Breakouts in Transversely Isotropic Posidonia Shale T1 - Bohrlochrandausbrüche in transversal isotropen Posidonienschiefer N2 - Borehole instabilities are frequently encountered when drilling through finely laminated, organic rich shales (Økland and Cook, 1998; Ottesen, 2010; etc.); such instabilities should be avoided to assure a successful exploitation and safe production of the contained unconventional hydrocarbons. Borehole instabilities, such as borehole breakouts or drilling induced tensile fractures, may lead to poor cementing of the borehole annulus, difficulties with recording and interpretation of geophysical logs, low directional control and in the worst case the loss of the well. If these problems are not recognized and expertly remedied, pollution of the groundwater or the emission of gases into the atmosphere can occur since the migration paths of the hydrocarbons in the subsurface are not yet fully understood (e.g., Davies et al., 2014; Zoback et al., 2010). In addition, it is often mentioned that the drilling problems encountered and the resulting downtimes of the wellbore system in finely laminated shales significantly increase drilling costs (Fjaer et al., 2008; Aadnoy and Ong, 2003). In order to understand and reduce the borehole instabilities during drilling in unconventional shales, we investigate stress-induced irregular extensions of the borehole diameter, which are also referred to as borehole breakouts. For this purpose, experiments with different borehole diameters, bedding plane angles and stress boundary conditions were performed on finely laminated Posidonia shales. The Lower Jurassic Posidonia shale is one of the most productive source rocks for conventional reservoirs in Europe and has the greatest potential for unconventional oil and gas in Europe (Littke et al., 2011). In this work, Posidonia shale specimens from the North (PN) and South (PS) German basins were selected and characterized petrophysically and mechanically. The composition of the two shales is dominated by calcite (47-56%) followed by clays (23-28%) and quartz (16-17%). The remaining components are mainly pyrite and organic matter. The porosity of the shales varies considerably and is up to 10% for PS and 1% for PN, which is due to a larger deposition depth of PN. Both shales show marked elasticity and strength anisotropy, which can be attributed to a macroscopic distribution and orientation of soft and hard minerals. Under load the hard minerals form a load-bearing, supporting structure, while the soft minerals compensate the deformation. Therefore, if loaded parallel to the bedding, the Posidonia shale is more brittle than loaded normal to the bedding. The resulting elastic anisotropy, which can be defined by the ratio of the modulus of elasticity parallel and normal to the bedding, is about 50%, while the strength anisotropy (i.e., the ratio of uniaxial compressive strength normal and parallel to the bedding) is up to 66%. Based on the petrophysical characterization of the two rocks, a transverse isotropy (TVI) was derived. In general, PS is softer and weaker than PN, which is due to the stronger compaction of the material due to the higher burial depth. Conventional triaxial borehole breakout experiments on specimens with different borehole diameters showed that, when the diameter of the borehole is increased, the stress required to initiate borehole breakout decreases to a constant value. This value can be expressed as the ratio of the tangential stress and the uniaxial compressive strength of the rock. The ratio increases exponentially with decreasing borehole diameter from about 2.5 for a 10 mm diameter hole to ~ 7 for a 1 mm borehole (increase of initiation stress by 280%) and can be described by a fracture mechanic based criterion. The reduction in borehole diameter is therefore a considerable aspect in reducing the risk of breakouts. New drilling techniques with significantly reduced borehole diameters, such as "fish-bone" holes, are already underway and are currently being tested (e.g., Xing et al., 2012). The observed strength anisotropy and the TVI material behavior are also reflected in the observed breakout processes at the borehole wall. Drill holes normal to the bedding develop breakouts in a plane of isotropy and are not affected by the strength or elasticity anisotropy. The observed breakouts are point-symmetric and form compressive shear failure planes, which can be predicted by a Mohr-Coulomb failure approach. If the shear failure planes intersect, conjugate breakouts can be described as "dog-eared” breakouts. While the initiation of breakouts for wells oriented normal to the stratification has been triggered by random local defects, reduced strengths parallel to bedding planes are the starting point for breakouts for wells parallel to the bedding. In the case of a deflected borehole trajectory, therefore, the observed failure type changes from shear-induced failure surfaces to buckling failure of individual layer packages. In addition, the breakout depths and widths increased, resulting in a stress-induced enlargement of the borehole cross-section and an increased output of rock material into the borehole. With the transition from shear to buckling failure and changing bedding plane angle with respect to the borehole axis, the stress required for inducing wellbore breakouts drops by 65%. These observations under conventional triaxial stress boundary conditions could also be confirmed under true triaxial stress conditions. Here breakouts grew into the rock as a result of buckling failure, too. In this process, the broken layer packs rotate into the pressure-free drill hole and detach themselves from the surrounding rock by tensile cracking. The final breakout shape in Posidonia shale can be described as trapezoidal when the bedding planes are parallel to the greatest horizontal stress and to the borehole axis. In the event that the largest horizontal stress is normal to the stratification, breakouts were formed entirely by shear fractures between the stratification and required higher stresses to initiate similar to breakouts in conventional triaxial experiments with boreholes oriented normal to the bedding. In the content of this work, a fracture mechanics-based failure criterion for conventional triaxial loading conditions in isotropic rocks (Dresen et al., 2010) has been successfully extended to true triaxial loading conditions in the transverse isotropic rock to predict the initiation of borehole breakouts. The criterion was successfully verified on the experiments carried out. The extended failure criterion and the conclusions from the laboratory and numerical work may help to reduce the risk of borehole breakouts in unconventional shales. N2 - Bei Bohrungen in feinlaminierten, organikreichen Schiefern werden häufig Bohrlochinstabilitäten beobachtet (Økland und Cook, 1998; Ottesen, 2010 und weitere), welche für eine sichere und erfolgreiche Erschließung der darin gespeicherten unkonventionellen Kohlenwasserstoffe vermieden werden sollten. Bohrlochinstabilitäten, wie zum Beispiel Bohrlochrandausbrüche oder bohrungsbedingte Zugrisse, führen unter Umständen zu einer schlechten bzw. unzureichenden Zementierung des Ringraum, zu Schwierigkeiten bei der Aufnahme und späteren Interpretation bohrlochgeophysikalischer Messungen sowie zu einer verringerten Kontrolle über die Auslenkung der Bohrung und im schlimmsten Fall zum Verlust der Bohrung. Werden diese Probleme nicht erkannt und fachmännisch behoben, kann es zur Verschmutzung des Grundwassers oder zum Austritt von Gasen in die Atmosphäre kommen, da die Migrationspfade der Kohlenwasserstoffe im Untergrund noch nicht vollständig verstanden sind (z.B. Davies et al., 2014; Zoback et al., 2010). Darüber hinaus wird häufig erwähnt, dass die angetroffenen Bohrprobleme und die daraus entstehenden Ausfallzeiten der Bohrlochanlage in feinlaminierten Schiefern die Bohrkosten erheblich erhöhen (Fjaer et al., 2008; Aadnoy und Ong, 2003). Um die Bohrlochinstabilitäten während des Bohrens in unkonventionellen Speichergesteinen zu verstehen und zu reduzieren, untersuchen wir in dieser Arbeit spannungsbedingte unregelmäßige Erweiterungen des Bohrlochdurchmessers, die auch als Bohrlochrandausbrüche (borehole breakouts) bezeichnet werden. Dazu wurden Versuche mit unterschiedlichen Bohrlochdurchmessern, Schichteinfallswinkeln und Belastungsrandbedingungen an feinlaminierten Posidonienschiefern durchgeführt. Der aus dem Unteren Jura stammende Posidonienschiefer ist eines der produktivsten Muttergesteine für konventionelle Lagerstätten in Europa und besitzt zeitgleich das größte Potential für unkonventionelles Öl und Gas in Europa (Littke et al., 2011). Im Rahmen dieser Arbeit wurden Posidonienschieferproben aus dem Norddeutschen (PN) und Süddeutschen (PS) Becken ausgewählt und petrophysikalisch sowie mechanisch charakterisiert. Die Zusammensetzung der beiden Schiefer wird dominiert von Kalzit (47-56%) gefolgt von Tonen (23-28%) und Quarz (16-17%). Die verbleibenden Komponenten sind hauptsächlich Pyrit und organische Substanz. Die Porosität des Schiefers schwankt beträchtlich und beträgt bis zu 10% für PS und 1% für PN, was auf eine größere Versenkungstiefe von PN zurückzuführen ist. Beide Schiefer zeigen ausgeprägte Elastizitäts- und Festigkeitsanisotropie, welche einer makroskopischen Verteilung und Orientierung von weichen und harten Mineralen zugeschrieben werden kann. Unter Belastung bilden die harten Minerale eine tragende Struktur, während die weichen Minerale die Verformung kompensieren. Daher verhält sich der Posidonienschiefer bei Belastung parallel zur Schichtfläche spröder als bei einer Belastung normal zur Schichtfläche. Die resultierende elastische Anisotropie, die über das Verhältnis des Elastizitätsmoduls parallel und normal zu Schichtung definiert werden kann, beträgt circa 50%, während die Festigkeitsanisotropie (d.h. das Verhältnis der uniaxialen Druckfestigkeit normal und parallel zur Schichtung) bis zu 66% beträgt. Basierend auf der petrophysikalischen Charakterisierung der beiden Gesteine konnte eine transversale Isotropie (TVI) abgeleitet werden. Im Allgemeinen ist PS weicher und schwächer als PN, was auf der stärkeren Verdichtung des Materials aufgrund der höheren Versenkungstiefe beruht. Konventionelle triaxiale Experimente zur Entstehung von Bohrlochrandausbrüchen an Proben mit unterschiedlichen Bohrlochdurchmessern zeigten, dass bei Vergrößerung des Bohrlochdurchmessers die zum Auslösen des Randausbruches erforderliche Spannung gegen einen konstanten Wert absinkt. Dieser kann als Verhältnis der Tangentialspannung und der einachsialen Druckfestigkeit des Gesteins ausgedrückt werden. Das Verhältnis erhöht sich exponentiell mit kleiner werdendem Bohrlochdurchmesser von circa 2,5 für ein 10 mm großes Bohrloch auf ~7 für ein 1 mm großes Bohrloch (Zunahme der Initiierungsspannung um 280%) und kann durch ein bruchmechanisch basiertes Kriterium beschrieben werden. Die Verringerung des Bohrlochdurchmessers stellt daher einen beträchtlichen Aspekt bei der Verringerung des Risikos für Bohrlochausbrüche dar. Neue Bohrtechniken mit deutlich reduzierten Bohrlochdurchmessern wie zum Beispiel „fish-bone“ Bohrungen nehmen dieses Konzept bereits auf und werden derzeit getestet (z. B. Xing et al., 2012). Die beobachtete Festigkeitsanisotropie und das TVI Materialverhalten spiegeln sich auch in den beobachteten Ausbruchsprozessen am Bohrlochrand wider. Bohrlöcher normal zur Schichtung entwickeln Randausbrüche in einer Ebene der Isotropie und werden nicht durch die Festigkeitsoder Elastizitätsanisotropie beeinflusst. Die beobachteten Ausbrüche sind punktsymmetrisch und bilden kompressive Schubversagensebenen, die durch einen Mohr-Coulomb-Versagensansatz vorhergesagt werden können. Falls sich die Schubversagensebenen schneiden, bilden sich konjugierte Ausbrüche die als „hundeohrförmig“ (dog-eared breakout) beschrieben werden können. Während die Initiierung von Randausbrüchen für Bohrlöcher normal zur Schichtung durch zufällige lokale Defekte ausgelöst wurde, sind reduzierte Festigkeiten parallel zur Schichtung der Ausgangspunkt für Bohrlochrandausbrüche für Bohrlöcher parallel zur Schichtung. Im Falle einer abgelenkten Bohrlochtrajektorie ändert sich daher der beobachtete Versagenstyp von schubdominiertem Versagensflächen zu Knickversagen einzelner Schichtpakete. Darüber hinaus nahmen die Ausbruchtiefen und -breiten zu, was zu einer spannungsbedingten Vergrößerung des Bohrlochquerschnitts und einem vermehrten Ausstoß von Gesteinsmaterial in das Bohrloch führte. Zeitgleich sinkt beim Übergang von Schub- zu Knickversagen und sich ändernden Schichteinfallswinkel, die für das Induzieren von Bohrlochrandausbrüchen notwendige Spannung um 65%, deutlich ab. Diese Beobachtungen unter konventionellen triaxialen Belastungsrandbedingungen konnten auch unter echt-triaxialen Belastungsrandbedingungen bestätigt werden. Hier wuchsen die Randausbrüche ebenfalls normal zur Schichtfläche durch Knickfehler in das Gestein. Dabei rotierten die gebrochenen Schichtpakete in das druckfreie Bohrloch und lösten sich vom umgebenden Gestein durch Zugrisse ab. Die endgültige Ausbruchform im Posidonienschiefer kann als trapezförmig beschrieben werden, wenn die Schichtfläche parallel zur größten horizontalen Spannung liegt. In dem Fall, dass die größte horizontale Spannung normal zur Schichtung orientiert ist, wurden Ausbrüche vollständig durch Scherbrüche zwischen den Schichtflächen gebildet und benötigten höhere Spannungen zur Initiierung. Im Rahmen dieser Arbeit wurde ein bruchmechanisch-basiertes Versagenskriterium für konventionelle triaxiale Belastungsbedingungen in isotropen Gesteinen (Dresen et al., 2010) erfolgreich auf echte triaxiale Belastungsbedingungen im transversal isotropen Gestein erweitert, um die Initiierung von Bohrlochrandausbrüchen vorherzusagen. Das Kriterium konnte erfolgreich an den durchgeführten Versuchen verifiziert werden. Das erweiterte Versagenskriterium und die Schlussfolgerungen aus dem Labor und der numerischen Arbeit helfen, das Risiko von Bohrlochausbrüchen in unkonventionellen Schiefern zu reduzieren. KW - borehole breakouts KW - unconventional shale KW - Posidonia shale KW - hollow cylinder experiments KW - shale strength KW - Bohrlochrandausbrüche KW - unkonventionelle Schiefer KW - Posidonienschiefer KW - Hohlzylinderversuche KW - Festigkeit des Schiefer Y1 - 2017 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-400019 ER - TY - JOUR A1 - Hammer, Conny A1 - Fäh, Donat A1 - Ohrnberger, Matthias T1 - Automatic detection of wet-snow avalanche seismic signals JF - Natural hazards : journal of the International Society for the Prevention and Mitigation of Natural Hazards N2 - Avalanche activity is an important factor when estimating the regional avalanche danger. Moreover, a complete and detailed picture of avalanche activity is needed to understand the processes that lead to natural avalanche release. Currently, information on avalanche activity is mainly obtained through visual observations. However, this involves large uncertainties in the number and release times, influencing the subsequent analysis. Therefore, alternative methods for the remote detection of snow avalanches in particular in non-observed areas are highly desirable. In this study, we use the excited ground vibration to identify avalanches automatically. The specific seismic signature of avalanches facilitates the objective detection by a recently developed classification procedure. A probabilistic description of the signals, called hidden Markov models, allows the robust identification of corresponding signals in the continuous data stream. The procedure is based upon learning a general background model from continuous seismic data. Then, a single reference waveform is used to update an event-specific classifier. Thus, a minimum amount of training data is required by constructing such a classifier on the fly. In this study, we processed five days of continuous data recorded in the Swiss Alps during the avalanche winter 1999. With the restriction of testing large wet-snow avalanches only, the presented approach achieved very convincing results. We successfully detect avalanches over a large volume and distance range. Ninety-two percentage of all detections (43 out of 47) could be confirmed as avalanche events; only four false alarms are reported. We see a clear dependence of recognition capability on run-out distance and source-receiver distance of the observed events: Avalanches are detectable up to a source-receiver distance of eight times the avalanche length. Implications for analyzing a more comprehensive data set (smaller events and different flow regimes) are discussed in detail. KW - Snow avalanche recognition KW - Automatic detection KW - Avalanche forecasting KW - Hidden Markov model Y1 - 2016 U6 - https://doi.org/10.1007/s11069-016-2707-0 SN - 0921-030X SN - 1573-0840 VL - 86 SP - 601 EP - 618 PB - Springer CY - New York ER - TY - THES A1 - Weege, Stefanie T1 - Climatic drivers of retrogressive thaw slump activity and resulting sediment and carbon release to the nearshore zone of Herschel Island, Yukon Territory, Canada T1 - Einfluss des Klimas auf das Auftauen einer rückschreitenden Erosionsfront und die daraus resultierende Sediment- und Kohlenstofffreigabe in den Küstenbereich von Herschel Island, Kanada N2 - The Yukon Coast in Canada is an ice-rich permafrost coast and highly sensitive to changing environmental conditions. Retrogressive thaw slumps are a common thermoerosion feature along this coast, and develop through the thawing of exposed ice-rich permafrost on slopes and removal of accumulating debris. They contribute large amounts of sediment, including organic carbon and nitrogen, to the nearshore zone. The objective of this study was to 1) identify the climatic and geomorphological drivers of sediment-meltwater release, 2) quantify the amount of released meltwater, sediment, organic carbon and nitrogen, and 3) project the evolution of sediment-meltwater release of retrogressive thaw slumps in a changing future climate. The analysis is based on data collected over 18 days in July 2013 and 18 days in August 2012. A cut-throat flume was set up in the main sediment-meltwater channel of the largest retrogressive thaw slump on Herschel Island. In addition, two weather stations, one on top of the undisturbed tundra and one on the slump floor, measured incoming solar radiation, air temperature, wind speed and precipitation. The discharge volume eroding from the ice-rich permafrost and retreating snowbanks was measured and compared to the meteorological data collected in real time with a resolution of one minute. The results show that the release of sediment-meltwater from thawing of the ice-rich permafrost headwall is strongly related to snowmelt, incoming solar radiation and air temperature. Snowmelt led to seasonal differences, especially due to the additional contribution of water to the eroding sediment-meltwater from headwall ablation, lead to dilution of the sediment-meltwater composition. Incoming solar radiation and air temperature were the main drivers for diurnal and inter-diurnal fluctuations. In July (2013), the retrogressive thaw slump released about 25 000 m³ of sediment-meltwater, containing 225 kg dissolved organic carbon and 2050 t of sediment, which in turn included 33 t organic carbon, and 4 t total nitrogen. In August (2012), just 15 600 m³ of sediment-meltwater was released, since there was no additional contribution from snowmelt. However, even without the additional dilution, 281 kg dissolved organic carbon was released. The sediment concentration was twice as high as in July, with sediment contents of up to 457 g l-1 and 3058 t of sediment, including 53 t organic carbon and 5 t nitrogen, being released. In addition, the data from the 36 days of observations from Slump D were upscaled to cover the main summer season of 1 July to 31 August (62 days) and to include all 229 active retrogressive thaw slumps along the Yukon Coast. In total, all retrogressive thaw slumps along the Yukon Coast contribute a minimum of 1.4 Mio. m³ sediment-meltwater each thawing season, containing a minimum of 172 000 t sediment with 3119 t organic carbon, 327 t nitrogen and 17 t dissolved organic carbon. Therefore, in addition to the coastal erosion input to the Beaufort Sea, retrogressive thaw slumps additionally release 3 % of sediment and 8 % of organic carbon into the ocean. Finally, the future evolution of retrogressive thaw slumps under a warming scenario with summer air temperatures increasing by 2-3 °C by 2081-2100, would lead to an increase of 109-114% in release of sediment-meltwater. It can be concluded that retrogressive thaw slumps are sensitive to climatic conditions and under projected future Arctic warming will contribute larger amounts of thawed permafrost material (including organic carbon and nitrogen) into the environment. N2 - Die Yukon Küste in Kanada ist eine eisreiche Permafrost Küste und reagiert hoch sensibel auf verändernde Umweltbedingungen. Rückschreitende auftaubedingte Rutschungen sind vielzählig entlang der Küste und entstehen, wenn exponierter eisreicher Permafrost an Hängen auftaut und der daraus resultierende Schlamm abtransportiert wird. Diese Rutschungen tragen große Mengen von Sediment, inklusive organischen Kohlenstoff und Stickstoff, in den küstennahen Bereich. Das Ziel dieser Studie war 1) die klimatischen und geomorphologischen Antriebskräfte für die Freisetzung von Sediment-Schmelzwasser zu identifizieren 2) die Mengen an Schmelzwasser, Sediment, organischen Kohlenstoff und Stickstoff zu quantifizieren und 3) die Entwicklung der Sediment-Schmelzwasser-Freigabe von rückschreitenden Rutschungen unter zukünftigen klimatischen Veränderungen abzuschätzen. Die größte rückschreitende Rutschung auf Herschel Island wird als „Slump D“ bezeichnet und steht im Fokus dieser Arbeit. Die Analysen basierten auf den Daten, die über 18 Tage im Juli (2013) und 18 Tage im August (2012) erhoben wurden. Eine Abfluss-Messrinne wurde in den Haupt-Sediment-Schmelzwasser-Kanal eingebaut, um die Sediment-Schmelzwassermassen zu erfassen. Zusätzlich wurden zwei Wetterstationen aufgebaut (auf der unberührten Tundra und innerhalb der Erosionsfläche), die Sonneneinstrahlung, Lufttemperatur, Windgeschwindigkeit und Niederschlagsmenge aufzeichneten. Das Abflussvolumen, das vom auftauenden, eisreichen Permafrost und den schmelzenden Schneebänken ablief, wurde gemessen und mit den meteorologischen Daten in Echtzeit mit einer Auflösung von einer Minute verglichen. Die Ergebnisse zeigen, dass eine Freigabe von Sediment-Schmelzwasser beim Auftauen der eisreichen Permafrost-Steilklippe stark von Schneeschmelze, Sonneneinstrahlung und Lufttemperatur abhängen. Die Schneeschmelze führt zu saisonalen Unterschieden, besonders durch den zusätzlichen Betrag von Wasser zu dem erodierenden Sediment-Schmelzwasser der auftauenden Steilklippe. Dies führt zu einer Verdünnung des Sediment-Schmelzwassers. Sonneneinstrahlung und Lufttemperaturen waren die Hauptantriebskräfte für die Schwankungen im Tagesverlauf und die Unterschiede zwischen den Tagen. Die rückschreitende Rutschung gab im Juli (2013) ungefähr 25 000 m³ Sediment-Schmelzwasser frei, welches 225 kg gelösten organischen Kohlenstoff, 2050 t Sediment, inklusive 33 t organischen Kohlenstoff und 4 t Stickstoff enthielt. Im August (2012) fehlte der zusätzliche Eintrag der Schneeschmelze und das Sediment-Schmelzwasser-Volumen war geringer mit 15 600 m³. Dennoch, ohne die zusätzliche Verdünnung, wurden 281 kg gelöster organischer Kohlenstoff freigesetzt. Die Sedimentkonzentration war doppelt so hoch und führte zu einem Sedimentgehalt mit bis zu 457 g l-1 zu 3058 t Sediment, inklusive 53 t organischen Kohlenstoff und 5 t Stickstoff. Zusätzlich wurden die Daten der 36-tägigen Abflussmessung der rückschreitenden Rutschung auf 62 Tage, von 1. Juli bis 31. August auf alle 229 aktiven Rutschungen entlang der Yukon Küste hochgerechnet. Es wurde diskutiert, dass alle rückschreitenden Rutschungen entlang der Yukon Küste zusammen mindestens 1,4 Mio. m³ Sediment-Schmelzwasser während jeder Auftausaison freigeben. Diese enthalten ein Minimum von 172 000 t Sediment, 3119 t organischen Kohlenstoff, 327 t Stickstoff und 17 t gelösten organischen Kohlenstoff. Daher kann zusammengefasst werden, dass zusätzlich zur Küstenerosion von allen Rutschungen noch ein zusätzlicher Beitrag von 3 % Sediment und 8 % organischen Kohlenstoff in die Beaufort See eingetragen wird. Schließlich wurde die zukünftige Entwicklung dieser rückschreitenden Rutschungen bei einem Temperaturanstieg von 2-3 °C bis 2081-2100 diskutiert. Dies könnte zu einem Anstieg der Sediment-Schmelzwasser-Freigabe von 109-114 % führen. Es kann daraus geschlossen werden, dass rückschreitende Rutschungen sensibel auf Klimabedingungen reagieren und mit der Arktischen Erwärmung größere Mengen an auftauenden Permafrost (inklusive organischen Kohlenstoff und Stickstoff) in die Umwelt freigeben werden. KW - permafrost KW - arctic KW - Canada KW - coast KW - erosion KW - Permafrost KW - Arktik KW - Kanada KW - Küste KW - Erosion Y1 - 2017 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-397947 ER - TY - THES A1 - Korzeniowska, Karolina T1 - Object-based image analysis for detecting landforms diagnostic of natural hazards T1 - Objektbasierte Bildanalyse zur Erfassung spezieller diagnostischer Landformen von Naturgefahren N2 - Natural and potentially hazardous events occur on the Earth’s surface every day. The most destructive of these processes must be monitored, because they may cause loss of lives, infrastructure, and natural resources, or have a negative effect on the environment. A variety of remote sensing technologies allow the recoding of data to detect these processes in the first place, partly based on the diagnostic landforms that they form. To perform this effectively, automatic methods are desirable. Universal detection of natural hazards is challenging due to their differences in spatial impacts, timing and longevity of consequences, and the spatial resolution of remote-sensing data. Previous studies have reported that topographic metrics such as roughness, which can be captured from digital elevation data, can reveal landforms diagnostic of natural hazards, such as gullies, dunes, lava fields, landslides and snow avalanches, as these landforms tend to be more heterogeneous than the surrounding landscape. A single roughness metric is often limited in such detections; however, a more complex approach that exploits the spatial relation and the location of objects, such as object-based image analysis (OBIA), is desirable. In this thesis, I propose a topographic roughness measure derived from an airborne laser scanning (ALS) digital terrain model (DTM) and discuss its performance in detecting landforms principally diagnostic of natural hazards. I further develop OBIA-based algorithms for the detection of snow avalanches using near-infrared (NIR) aerial images, and the size (changes) of mountain lakes using LANDSAT satellite images. I quantitatively test and document how the level of difficulty in detecting these very challenging landforms depends on the input data resolution, the derivatives that could be evaluated from images and DTMs, the size, shape and complexity of landforms, and the capabilities of obtaining the information in the data. I demonstrate that surface roughness is a promising metric for detecting different landforms in diverse environments, and that OBIA assists significantly in detecting parts of lakes and snow avalanches that may not be correctly assigned by applying only the thresholding of spectral properties of data and their derivatives. The curvature-based surface roughness parameter allows the detection of gullies, dunes, lava fields and landslides with a user’s accuracy of 0.63, 0.21, 0.53, and 0.45, respectively. The OBIA algorithms for detecting lakes and snow avalanches obtained user’s accuracy of 0.98, and 0.78, respectively. Most of the analysed landforms constituted only a small part of the entire dataset, and therefore the user’s accuracy is the most appropriate performance measure that should be given in a such classification, because it tells how many automatically-extracted pixels in fact represent the object that one wants to classify, and its calculation does not take the second (background) class into account. One advantage of the proposed roughness parameter is that it allows the extraction of the heterogeneity of the surface without the need for data detrending. The OBIA approach is novel in that it allows the classification of lakes regardless of the physical state of their water, and also allows the separation of frozen lakes from glaciers that have very similar water indices used in purely optical remote sensing applications. The algorithm proposed for snow avalanches allows the detection of release zones, tracks, and deposition zones by verifying the snow heterogeneity based on a roughness metric evaluated from a water index, and by analysing the local relation of segments with their neighbouring objects. This algorithm contains few steps, which allows for the simultaneous classification of avalanches that occur on diverse mountain slopes and differ in size and shape. This thesis contributes to natural hazard research as it provides automatic solutions to tracking six different landforms that are diagnostic of natural hazards over large regions. This is a step toward delineating areas susceptible to the processes producing these landforms and the improvement of hazard maps. N2 - Naturgefahren und potenziell gefährliche Ereignisse der Erdoberfläche treten jeden Tag auf. Prozesse mit Zerstörungswirkungen sollten identifiziert werden, weil sie Gefahren für besiedelte Gebiete sowie menschliches Leben haben können. Naturgefahren haben erhebliche Einflüsse auf die Umwelt. Eine Vielzahl von Fernerkundungstechnologien, die heutzutage verfügbar sind, erlauben die Aufnahme und Speicherung von Datensätzen, die bei der Erkennung solcher Naturgefahren helfen können. Eine wichtige Grundlage dafür stellt die diagnostische Landform dar, welche die Naturgefahr ausbildet. Für eine effiziente Analyse sind automatische Methoden wünschenswert. Die Verwendung einer universellen Methode zur Erkennung von Naturgefahren ist deshalb eine Herausforderung, weil die räumlichen Ausdehnungen unterschiedlich sind. So können diese unterschiedlichen Alters sein und verschiedene räumliche Auflösungen in Fernerkundungsdaten besitzen. Dies beeinflusst den Detailierungsgrad bei der Abbildung der Erdoberfläche. Frühere Studien zeigen, dass Ableitungen wie beispielweise die Rauheit, die von Fernerkundungsdaten erfasst werden kann, es erlauben, Naturgefahrenphänomene wie z. B. Erosionsrinnen, Dünen, Lavafelder, Erdrutsche und Schneelawinen zu erkennen, weil sie heterogener sind als umgebende Objekte. Dennoch ist es nicht zulässig, allein mittels der eigenständigen Rauheit eine Unterscheidung zwischen den erfassten Landschaftsformen vorzunehmen. Hier ist ein komplexer Ansatz wie die Objektbasierte Bildanalyse (OBIA) wünschenswert, weil ein solcher sowohl die räumliche Relation als auch die Lage von Objekten verwendet. In dieser Dissertation schlage ich einen Oberflächenrauhigkeitsindex, abgeleitet aus einem durch Airborne Laserscanning (ALS) erfassten digitalen Geländemodells (DTM), vor und diskutiere die Faktoren, die die Darstellung von Naturgefahrenphänomenen mittels dieser Variable beeinflussen. Ich präsentiere auch OBIA-basierte, automatische Algorithmen für die Erkennung von Schneelawinen welche aus Nah-Infrarot (NIR) Luftbildern ausgewertet wurden sowie den Verlauf einer Seegrenze, die auf LANDSAT Satellitenbildern abgebildet wird. Ich zeige weiterhin, dass der Schwierigkeitsgrad für die Erfassung der analysierten Phänomene variabel und abhängig von den Dateneigenschaften, der Komplexität der getrackten Phänomene sowie von den qualitativen Ausprägungen des Informationsgehaltes ist. Ferner werde ich zeigen, dass die vorgeschlagene Oberflächenrauhigkeit die räumliche Ausdehnung der verschiedenen Phänomene zu bestimmen erlaubt, und dass der OBIA-Ansatz deutlich bei der Erkennung von Objekten und derjenigen Teile hilft, die nicht korrekt nur durch Verwendung spektraler Eigenschaften von Daten und deren Derivaten zugewiesen werden konnten. Der krümmungsbasierte Oberflächenrauhigkeitindex ermöglicht die Erkennung von Erosionsrinnen, Dünen, Lavafeldern, und Erdrutschen mit einer Benutzergenauigkeit von: 0.63, 0.21, 0.53 und 0.45. Vergleichend dazu erzielen die vorgestellten OBIA-Algorithmen für die Erfassung von Seen und Schneelawinen eine Benutzergenauigkeit von 0.98 und 0.78. Die in dieser Arbeit analysierten Landformen stellen einen Ausschnitt aus dem Gesamtspektrum vorkommender Strukturen dar. Die Benutzergenauigkeit stellt dabei den am besten geeigneten Leistungsindex dar, auf dem basierend eine Klassifikation durchgeführt werden kann. Die Benutzergenauigkeit gibt an, wie viele der automatisch extrahierten Pixel das zu klassifizierende Objekt tatsächlich repräsentieren. Eine Betrachtung einer zweiten (Hintergrund-) Klasse muss durch diesen Ansatz nicht erfolgen. Ein Vorteil des vorgeschlagenen Oberflächenrauhigkeitindex ist, dass er die Extraktion der Heterogenität der Oberfläche ohne die Notwendigkeit eines Daten-detrendings ermöglicht. Der OBIA-Ansatz für die Erfassung von Seegrenzen erlaubt es einerseits, Seen ungeachtet der physikalischen Zustände des Wassers zu klassifizieren und anderseits gefrorene Seen von den Gletschern zu unterschieden, welche ähnliche Eigenschaften beim Wasserindex aufweisen. Der für Schneelawinen vorgeschlagene Algorithmus wiederum ermöglicht insgesamt die Erfassung von Anbruchgebieten, Sturzbahnen und Ablagerungszonen durch Verifikation der Schneeheterogenität sowie die lokalen Beziehungen zu benachbarten Objekten. Dieser Algorithmus enthält einige Schritte, die es erlauben, gleichzeitig Lawinen zu klassifizieren, die in verschiedenen Berghängen auftreten und unterschiedliche Größen und Formen haben. Diese Dissertation trägt zur Naturgefahrenforschung bei, da sie automatische Lösungen für das Monitoring von sechs verschiedenen Landformen bietet, die typisch für Naturgefahren sind. Es wird somit dazu beigetragen, Gebiete abgrenzbar zu machen, welche für das Auftreten von Gefahrenphänomenen besonders anfällig sind. Zudem können damit auch Verbesserungen bei der Erstellung von Gefahrenkarten erreicht werden. KW - object based image analysis KW - automatic classification KW - GIS KW - satellite images KW - photogrammetry KW - landforms KW - natural hazards KW - snow avalanches KW - lakes KW - roughness KW - objektbasierte Bildanalyse KW - automatische Klassifizierung KW - GIS KW - Satellitenbilder KW - Photogrammetrie KW - Landformen KW - Naturgefahren KW - Lawinen KW - Seen KW - Rauheit Y1 - 2017 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-402240 ER - TY - JOUR A1 - Mohr, Christian Heinrich A1 - Korup, Oliver A1 - Ulloa, Hector A1 - Iroume, Andres T1 - Pyroclastic Eruption Boosts Organic Carbon Fluxes Into Patagonian Fjords JF - Global biogeochemical cycles N2 - Fjords and old-growth forests store large amounts of organic carbon. Yet the role of episodic disturbances, particularly volcanic eruptions, in mobilizing organic carbon in fjord landscapes covered by temperate rainforests remains poorly quantified. To this end, we estimated how much wood and soils were flushed to nearby fjords following the 2008 eruption of Chaiten volcano in south-central Chile, where pyroclastic sediments covered >12km(2) of pristine temperate rainforest. Field-based surveys of forest biomass, soil organic content, and dead wood transport reveal that the reworking of pyroclastic sediments delivered similar to 66,500+14,600/-14,500tC of large wood to two rivers entering the nearby Patagonian fjords in less than a decade. A similar volume of wood remains in dead tree stands and buried beneath pyroclastic deposits (similar to 79,900+21,100/-16,900tC) or stored in active river channels (5,900-10,600tC). We estimate that bank erosion mobilized similar to 132,300(+21,700)/(-30,600)tC of floodplain forest soil. Eroded and reworked forest soils have been accreting on coastal river deltas at >5mmyr(-1) since the eruption. While much of the large wood is transported out of the fjord by long-shore drift, the finer fraction from eroded forest soils is likely to be buried in the fjords. We conclude that the organic carbon fluxes boosted by rivers adjusting to high pyroclastic sediment loads may remain elevated for up to a decade and that Patagonian temperate rainforests disturbed by excessive loads of pyroclastic debris can be episodic short-lived carbon sources. Plain Language Summary Fjords and old-growth forests are important sinks of organic carbon. However, the role of volcanic eruptions in flushing organic carbon in fjord landscapes remains unexplored. Here we estimated how much forest vegetation and soils were lost to fjords following the 2008 eruption ofunknownChaiten volcano in south-central Chile. Pyroclastic sediments obliterated near-pristine temperateunknownrainforest, and the subsequent reworking of these sediments delivered in less than a decade similar to 66,000 tC of large wood to the mountain rivers, draining into the nearby Patagonian fjords. A similar volume of wood remains in dead tree stands and buried beneath pyroclastic deposits or stored in active riverunknownchannels. We estimate that similar to 130,000 tC of organic carbon-rich soil was lost to erosion, thus adding to the carbon loads. While much of the wood enters the long-shore drift in the fjord heads, the finerunknownfraction from eroded forest soils is likely to be buried in the fjords at rates that exceed regional estimates by an order of magnitude. We anticipate that these eruption-driven fluxes will remain elevated forunknownthe coming years and that Patagonian temperate rainforests episodically switch from carbon sinks to hitherto undocumented carbon sources if disturbed by explosive volcanic eruptions. KW - Chile KW - Patagonia KW - rainforest KW - volcanic eruption KW - organic carbon KW - biomass Y1 - 2017 U6 - https://doi.org/10.1002/2017GB005647 SN - 0886-6236 SN - 1944-9224 VL - 31 SP - 1626 EP - 1638 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Korzeniowska, Karolina A1 - Buehler, Yves A1 - Marty, Mauro A1 - Korup, Oliver T1 - Regional snow-avalanche detection using object-based image analysis of near-infrared aerial imagery JF - Natural hazards and earth system sciences N2 - Snow avalanches are destructive mass movements in mountain regions that continue to claim lives and cause infrastructural damage and traffic detours. Given that avalanches often occur in remote and poorly accessible steep terrain, their detection and mapping is extensive and time consuming. Nonetheless, systematic avalanche detection over large areas could help to generate more complete and up-to-date inventories (cadastres) necessary for validating avalanche forecasting and hazard mapping. In this study, we focused on automatically detecting avalanches and classifying them into release zones, tracks, and run-out zones based on 0.25m near-infrared (NIR) ADS80-SH92 aerial imagery using an object-based image analysis (OBIA) approach. Our algorithm takes into account the brightness, the normalised difference vegetation index (NDVI), the normalised difference water index (NDWI), and its standard deviation (SDNDWI) to distinguish avalanches from other land-surface elements. Using normalised parameters allows applying this method across large areas. We trained the method by analysing the properties of snow avalanches at three 4km−2 areas near Davos, Switzerland. We compared the results with manually mapped avalanche polygons and obtained a user's accuracy of >0.9 and a Cohen's kappa of 0.79–0.85. Testing the method for a larger area of 226.3km−2, we estimated producer's and user's accuracies of 0.61 and 0.78, respectively, with a Cohen's kappa of 0.67. Detected avalanches that overlapped with reference data by >80% occurred randomly throughout the testing area, showing that our method avoids overfitting. Our method has potential for large-scale avalanche mapping, although further investigations into other regions are desirable to verify the robustness of our selected thresholds and the transferability of the method. Y1 - 2017 U6 - https://doi.org/10.5194/nhess-17-1823-2017 SN - 1561-8633 VL - 17 SP - 1823 EP - 1836 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Rosenwinkel, Swenja A1 - Landgraf, Angela A1 - Schwanghart, Wolfgang A1 - Volkmer, Friedrich A1 - Dzhumabaeva, Atyrgul A1 - Merchel, Silke A1 - Rugel, Georg A1 - Preusser, Frank A1 - Korup, Oliver T1 - Late Pleistocene outburst floods from Issyk Kul, Kyrgyzstan? JF - Earth surface processes and landforms : the journal of the British Geomorphological Research Group KW - outburst flood KW - lake-level changes KW - Issyk Kul KW - Kyrgyzstan KW - cosmogenic nuclides Y1 - 2017 U6 - https://doi.org/10.1002/esp.4109 SN - 0197-9337 SN - 1096-9837 VL - 42 SP - 1535 EP - 1548 PB - Wiley CY - Hoboken ER - TY - JOUR A1 - Korzeniowska, Karolina A1 - Korup, Oliver T1 - Object-Based Detection of Lakes Prone to Seasonal Ice Cover on the Tibetan Plateau JF - Remote sensing KW - Tibetan Plateau KW - lakes KW - LANDSAT KW - SRTM KW - MNDWI KW - OBIA KW - change detection Y1 - 2017 U6 - https://doi.org/10.3390/rs9040339 SN - 2072-4292 VL - 9 PB - MDPI CY - Basel ER - TY - JOUR A1 - Ziegler, Moritz O. A1 - Heidbach, Oliver A1 - Zang, Arno A1 - Martinez-Garzon, Patricia A1 - Bohnhoff, Marco T1 - Estimation of the differential stress from the stress rotation angle in low permeable rock JF - Geophysical research letters N2 - Rotations of the principal stress axes are observed as a result of fluid injection into reservoirs. We use a generic, fully coupled 3-D thermo-hydro-mechanical model to investigate systematically the dependence of this stress rotation on different reservoir properties and injection scenarios. We find that permeability, injection rate, and initial differential stress are the key factors, while other reservoir properties only play a negligible role. In particular, we find that thermal effects do not significantly contribute to stress rotations. For reservoir types with usual differential stress and reservoir treatment the occurrence of significant stress rotations is limited to reservoirs with a permeability of less than approximately 10(-12)m(2). Higher permeability effectively prevents stress rotations to occur. Thus, according to these general findings, the observed principal stress axes rotation can be used as a proxy of the initial differential stress provided that rock permeability and fluid injection rate are known a priori. Y1 - 2017 U6 - https://doi.org/10.1002/2017GL073598 SN - 0094-8276 SN - 1944-8007 VL - 44 SP - 6761 EP - 6770 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Martínez-Garzón, Patricia A1 - Kwiatek, Grzegorz A1 - Bohnhoff, Marco A1 - Dresen, Georg T1 - Volumetric components in the earthquake source related to fluid injection and stress state JF - Geophysical research letters N2 - We investigate source processes of fluid-induced seismicity from The Geysers geothermal reservoir in California to determine their relation with hydraulic operations and improve the corresponding seismic hazard estimates. Analysis of 869 well-constrained full moment tensors (M-w 0.8-3.5) reveals significant non-double-couple components (>25%) for about 65% of the events. Volumetric deformation is governed by cumulative injection rates with larger non-double-couple components observed near the wells and during high injection periods. Source mechanisms are magnitude dependent and vary significantly between faulting regimes. Normal faulting events (M-w<2) reveal substantial volumetric components indicating dilatancy in contrast to strike-slip events that have a dominant double-couple source. Volumetric components indicating closure of cracks in the source region are mostly found for reverse faulting events with M-w>2.5. Our results imply that source processes and magnitudes of fluid-induced seismic events are strongly affected by the hydraulic operations, the reservoir stress state, and the faulting regime. KW - non-double-couple components KW - induced seismicity KW - geothermal KW - stress state KW - tensile opening KW - pore pressure Y1 - 2017 U6 - https://doi.org/10.1002/2016GL071963 SN - 0094-8276 SN - 1944-8007 VL - 44 IS - 2 SP - 800 EP - 809 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Mohr, Christian Heinrich A1 - Manga, Michael A1 - Wang, Chi-Yuen A1 - Korup, Oliver T1 - Regional changes in streamflow after a megathrust earthquake JF - Earth & planetary science letters N2 - Moderate to large earthquakes can increase the amount of water feeding stream flows, mobilizing excess water from deep groundwater, shallow groundwater, or the vadose zone. Here we examine the regional pattern of streamflow response to the Maule M8.8 earthquake across Chile's diverse topographic and hydro-climatic gradients. We combine streamflow analyses with groundwater flow modeling and a random forest classifier, and find that, after the earthquake, at least 85 streams had a change in flow. Discharge mostly increased () shortly after the earthquake, liberating an excess water volume of >1.1 km3, which is the largest ever reported following an earthquake. Several catchments had increased discharge of >50 mm, locally exceeding seasonal streamflow discharge under undisturbed conditions. Our modeling results favor enhanced vertical permeability induced by dynamic strain as the most probable process explaining the observed changes at the regional scale. Supporting this interpretation, our random forest classification identifies peak ground velocity and elevation extremes as most important for predicting streamflow response. Given the mean recurrence interval of ∼25 yr for >M8.0 earthquakes along the Peru–Chile Trench, our observations highlight the role of earthquakes in the regional water cycle, especially in arid environments. KW - Maule earthquake KW - streamflow response KW - permeability KW - groundwater flow modeling KW - earthquake hydrology Y1 - 2016 U6 - https://doi.org/10.1016/j.epsl.2016.11.013 SN - 0012-821X SN - 1385-013X VL - 458 SP - 418 EP - 428 PB - Elsevier CY - Amsterdam ER - TY - GEN A1 - Wang, Yongbo A1 - Herzschuh, Ulrike A1 - Liu, Xingqi A1 - Korup, Oliver A1 - Diekmann, Bernhard T1 - Reply to Chong Xu’s comment on: Wang, Yongbo; Herzschuh, Ulrike; Liu, Xingqi; Korup, Oliver; Diekmann, Bernhard: A high-resolution sedimentary archive from landslide-dammed Lake Mengda, north-eastern Tibetan Plateau. - Journal of Paleolimnology. - 51 (2014), S. 303 - 312 T2 - Journal of paleolimnolog Y1 - 2016 U6 - https://doi.org/10.1007/s10933-016-9937-8 SN - 0921-2728 SN - 1573-0417 VL - 57 SP - 163 EP - 164 PB - Springer CY - Dordrecht ER - TY - GEN A1 - Korzeniowska, Karolina A1 - Bühler, Yves A1 - Mauro, Marty A1 - Korup, Oliver T1 - Regional snow-avalanche detection using object-based image analysis of near-infrared aerial imagery N2 - Snow avalanches are destructive mass movements in mountain regions that continue to claim lives and cause infrastructural damage and traffic detours. Given that avalanches often occur in remote and poorly accessible steep terrain, their detection and mapping is extensive and time consuming. Nonetheless, systematic avalanche detection over large areas could help to generate more complete and up-to-date inventories (cadastres) necessary for validating avalanche forecasting and hazard mapping. In this study, we focused on automatically detecting avalanches and classifying them into release zones, tracks, and run-out zones based on 0.25 m near-infrared (NIR) ADS80-SH92 aerial imagery using an object-based image analysis (OBIA) approach. Our algorithm takes into account the brightness, the normalised difference vegetation index (NDVI), the normalised difference water index (NDWI), and its standard deviation (SDNDWI) to distinguish avalanches from other land-surface elements. Using normalised parameters allows applying this method across large areas. We trained the method by analysing the properties of snow avalanches at three 4 km−2 areas near Davos, Switzerland. We compared the results with manually mapped avalanche polygons and obtained a user's accuracy of > 0.9 and a Cohen's kappa of 0.79–0.85. Testing the method for a larger area of 226.3 km−2, we estimated producer's and user's accuracies of 0.61 and 0.78, respectively, with a Cohen's kappa of 0.67. Detected avalanches that overlapped with reference data by > 80 % occurred randomly throughout the testing area, showing that our method avoids overfitting. Our method has potential for large-scale avalanche mapping, although further investigations into other regions are desirable to verify the robustness of our selected thresholds and the transferability of the method. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 398 Y1 - 2017 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-403942 ER - TY - JOUR A1 - Korzeniowska, Karolina A1 - Bühler, Yves A1 - Marty, Mauro A1 - Korup, Oliver T1 - Regional snow-avalanche detection using object-based image analysis of near-infrared aerial imagery JF - Natural hazards and earth system sciences : NHESS N2 - Snow avalanches are destructive mass movements in mountain regions that continue to claim lives and cause infrastructural damage and traffic detours. Given that avalanches often occur in remote and poorly accessible steep terrain, their detection and mapping is extensive and time consuming. Nonetheless, systematic avalanche detection over large areas could help to generate more complete and up-to-date inventories (cadastres) necessary for validating avalanche forecasting and hazard mapping. In this study, we focused on automatically detecting avalanches and classifying them into release zones, tracks, and run-out zones based on 0.25 m near-infrared (NIR) ADS80-SH92 aerial imagery using an object-based image analysis (OBIA) approach. Our algorithm takes into account the brightness, the normalised difference vegetation index (NDVI), the normalised difference water index (NDWI), and its standard deviation (SDNDWI) to distinguish avalanches from other land-surface elements. Using normalised parameters allows applying this method across large areas. We trained the method by analysing the properties of snow avalanches at three 4 km−2 areas near Davos, Switzerland. We compared the results with manually mapped avalanche polygons and obtained a user's accuracy of > 0.9 and a Cohen's kappa of 0.79–0.85. Testing the method for a larger area of 226.3 km−2, we estimated producer's and user's accuracies of 0.61 and 0.78, respectively, with a Cohen's kappa of 0.67. Detected avalanches that overlapped with reference data by > 80 % occurred randomly throughout the testing area, showing that our method avoids overfitting. Our method has potential for large-scale avalanche mapping, although further investigations into other regions are desirable to verify the robustness of our selected thresholds and the transferability of the method. Y1 - 2017 U6 - https://doi.org/10.5194/nhess-17-1823-2017 SN - 1561-8633 VL - 17 SP - 1823 EP - 1836 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Stolle, Amelie A1 - Bernhardt, Anne A1 - Schwanghart, Wolfgang A1 - Hoelzmann, Philipp A1 - Adhikari, Basanta R. A1 - Fort, Monique A1 - Korup, Oliver T1 - Catastrophic valley fills record large Himalayan earthquakes, Pokhara, Nepal JF - Quaternary science reviews : the international multidisciplinary research and review journal KW - Catastrophic valley infill KW - Great Himalayan earthquakes KW - Radiocarbon age dating KW - Provenance analysis KW - Paleoseismology KW - Nepal Y1 - 2017 U6 - https://doi.org/10.1016/j.quascirev.2017.10.015 SN - 0277-3791 VL - 177 SP - 88 EP - 103 PB - Elsevier CY - Oxford ER - TY - JOUR A1 - Bubeck, Philip A1 - Kreibich, Heidi A1 - Penning-Rowsell, E. C. A1 - Botzen, W. J. Wouter A1 - de Moel, H. A1 - Klijn, F. T1 - Explaining differences in flood management approaches in Europe and in the USA - a comparative analysis JF - Journal of flood risk management N2 - Flood risk management in Europe and worldwide is not static but constantly in a state of flux. There has been a trend towards more integrated flood risk management in many countries. However, the initial situation and the pace and direction of change is very different in the various countries. In this paper, we will present a conceptual framework that seeks to explain why countries opt for different flood risk management portfolios. The developed framework utilises insights from a range of policy science concepts in an integrated way and considers, among others, factors such as geographical characteristics, the experience with flood disasters, as well as human behavioural aspects. KW - Flood risk management KW - impact KW - policy Y1 - 2017 U6 - https://doi.org/10.1111/jfr3.12151 SN - 1753-318X VL - 10 SP - 436 EP - 445 PB - Wiley CY - Hoboken ER - TY - THES A1 - Irrgang, Anna Maria T1 - Temporal and spatial dynamics of Arctic coastal changes and the resulting impacts: Yukon Territory, Canada Y1 - 2017 ER - TY - THES A1 - Tanski, George T1 - Fate of organic matter mobilized from eroding permafrost coasts Y1 - 2017 ER - TY - JOUR A1 - Fathizadeh, O. A1 - Hosseini, Seyed Mehrdad A1 - Zimmermann, Alexander A1 - Keim, R. F. A1 - Boloorani, A. Darvishi T1 - Estimating linkages between forest structural variables and rainfall interception parameters in semi-arid deciduous oak forest stands JF - The science of the total environment : an international journal for scientific research into the environment and its relationship with man N2 - An understanding of the relationship between canopy structure and the water balance is needed for predicting how forest structure changes affect rainfall partitioning and, consequently, water resources. The objective of this study was to predict rainfall interception (I) and canopy storage capacity (S) using canopy structure variables and to investigate how seasonal changes influence their relationship. The study was conducted in twelve 50 m x 50 m plots in the Zagros forest in the western Iranian state of Ilam, protected forests of Dalab region. Average cumulative I was 84.2mm, accounting for 10.2% of cumulative gross precipitation (GP) over a 1-year period. Using a regression based method, S averaged similar to 1 mm and 0.1 mm in the leafed and leafless periods, respectively. There were no relationships between tree density and I: GP or S, but I: GP and S increased with leaf area index, canopy cover fraction, basal area, tree height, and diameter at breast height in the leafed period. In addition, wood area index and canopy cover fraction were related to I: GP or S in the leafless period. (C) 2017 Elsevier B.V. All rights reserved. KW - Canopy storage capacity KW - Canopy structure KW - Rainfall interception KW - Quercus brantii KW - Zagros forests Y1 - 2017 U6 - https://doi.org/10.1016/j.scitotenv.2017.05.233 SN - 0048-9697 SN - 1879-1026 VL - 601 SP - 1824 EP - 1837 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Foti, Sebastiano A1 - Hollender, Fabrice A1 - Garofalo, Flora A1 - Albarello, Dario A1 - Asten, Michael A1 - Bard, Pierre-Yves A1 - Comina, Cesare A1 - Cornou, Cecile A1 - Cox, Brady A1 - Di Giulio, Giuseppe A1 - Forbriger, Thomas A1 - Hayashi, Koichi A1 - Lunedei, Enrico A1 - Martin, Antony A1 - Mercerat, Diego A1 - Ohrnberger, Matthias A1 - Poggi, Valerio A1 - Renalier, Florence A1 - Sicilia, Deborah A1 - Socco, Valentina T1 - Guidelines for the good practice of surface wave analysis BT - a product of the InterPACIFIC project JF - Bulletin of earthquake engineering : official publication of the European Association for Earthquake Engineering N2 - Surface wave methods gained in the past decades a primary role in many seismic projects. Specifically, they are often used to retrieve a 1D shear wave velocity model or to estimate the V-s,V-30 at a site. The complexity of the interpretation process and the variety of possible approaches to surface wave analysis make it very hard to set a fixed standard to assure quality and reliability of the results. The present guidelines provide practical information on the acquisition and analysis of surface wave data by giving some basic principles and specific suggestions related to the most common situations. They are primarily targeted to non-expert users approaching surface wave testing, but can be useful to specialists in the field as a general reference. The guidelines are based on the experience gained within the InterPACIFIC project and on the expertise of the participants in acquisition and analysis of surface wave data. KW - Rayleigh waves KW - MASW KW - Ambient vibration analysis KW - Site characterization KW - Shear wave velocity KW - V-S,V-30 Y1 - 2017 U6 - https://doi.org/10.1007/s10518-017-0206-7 SN - 1570-761X SN - 1573-1456 VL - 16 IS - 6 SP - 2367 EP - 2420 PB - Springer CY - Dordrecht ER - TY - THES A1 - Osei Tutu, Anthony T1 - Linking global mantle dynamics with lithosphere dynamics using the geoid, plate velocities and lithosphere stress state as constraints T1 - Verknüpfung der globalen Manteldynamik mit der Lithosphärendynamik, unter Berücksichtigung des Geoids, der Plattengeschwindigkeiten und des Spannungszustandes der Lithosphäre als Einschränkungen BT - lithosphere and mantle dynamics coupling N2 - Lithospheric plates move over the low viscosity asthenosphere balancing several forces. The driving forces include basal shear stress exerted by mantle convection and plate boundary forces such as slab pull and ridge push, whereas the resisting forces include inter-plate friction, trench resistance, and cratonic root resistance. These generate plate motions, the lithospheric stress field and dynamic topography which are observed with different geophysical methods. The orientation and tectonic regime of the observed crustal/lithospheric stress field further contribute to our knowledge of different deformation processes occurring within the Earth's crust and lithosphere. Using numerical models previous studies were able to identify major forces generating stresses in the crust and lithosphere which also contribute to the formation of topography as well as driving lithospheric plates. They showed that the first-order stress pattern explaining about 80\,\% of the stress field originates from a balance of forces acting at the base of the moving lithospheric plates due to convective flow in the underlying mantle. The remaining second-order stress pattern is due to lateral density variations in the crust and lithosphere in regions of pronounced topography and high gravitational potential, such as the Himalayas and mid-ocean ridges. By linking global lithosphere dynamics to deep mantle flow this study seeks to evaluate the influence of shallow and deep density heterogenities on plate motions, lithospheric stress field and dynamic topography using the geoid as a major constraint for mantle rheology. We use the global 3D lithosphere-asthenosphere model SLIM3D with visco-elasto-plastic rheology coupled at 300 km depth to a spectral model of mantle flow. The complexity of the lithosphere-asthenosphere component allows for the simulation of power-law rheology with creep parameters accounting for both diffusion and dislocation creep within the uppermost 300 km. First we investigate the influence of intra-plate friction and asthenospheric viscosity on present-day plate motions. Previous modelling studies have suggested that small friction coefficients (µ < 0.1, yield stress ~ 100 MPa) can lead to plate tectonics in models of mantle convection. Here we show that, in order to match present-day plate motions and net rotation, the frictional parameter must be less than 0.05. We are able to obtain a good fit with the magnitude and orientation of observed plate velocities (NUVEL-1A) in a no-net-rotation (NNR) reference frame with µ < 0.04 and minimum asthenosphere viscosity ~ 5*10e19 Pas to 10e20 Pas. Our estimates of net rotation (NR) of the lithosphere suggest that amplitudes ~ 0.1-0.2 °/Ma, similar to most observation-based estimates, can be obtained with asthenosphere viscosity cutoff values of ~ 10e19 Pas to 5*10e19 Pas and friction coefficient µ < 0.05. The second part of the study investigates further constraints on shallow and deep mantle heterogeneities causing plate motion by predicting lithosphere stress field and topography and validating with observations. Lithosphere stresses and dynamic topography are computed using the modelling setup and rheological parameters for prescribed plate motions. We validate our results with the World Stress Map 2016 (WSM2016) and the observed residual topography. Here we tested a number of upper mantle thermal-density structures. The one used to calculate plate motions is considered the reference thermal-density structure. This model is derived from a heat flow model combined with a sea floor age model. In addition we used three different thermal-density structures derived from global S-wave velocity models to show the influence of lateral density heterogeneities in the upper 300 km on model predictions. A large portion of the total dynamic force generating stresses in the crust/lithosphere has its origin in the deep mantle, while topography is largely influenced by shallow heterogeneities. For example, there is hardly any difference between the stress orientation patterns predicted with and without consideration of the heterogeneities in the upper mantle density structure across North America, Australia, and North Africa. However, the crust is dominant in areas of high altitude for the stress orientation compared to the all deep mantle contribution. This study explores the sensitivity of all the considered surface observables with regards to model parameters providing insights into the influence of the asthenosphere and plate boundary rheology on plate motion as we test various thermal-density structures to predict stresses and topography. N2 - Lithosphärenplatten bewegen sich über die niederviskose Asthenosphäre, wobei mehrere Kräfte im Gleichgewicht stehen. Die antreibenden Kräfte umfassen eine basale Schubspannung, die durch Mantelkonvektion verursacht wird, und Plattengrenzkräfte, wie z.B. slab pull und ridge push, während die widerstehenden Kräfte die Reibung zwischen Platten, Widerstand an Tiefseegräben sowie an den kratonischen Wurzeln umfassen. Diese Kräfte erzeugen Plattenbewegungen, das lithosphärische Spannungsfeld und die dynamische Topographie, die mit verschiedenen geophysikalischen Methoden beobachtet werden. Die Orientierung und das tektonische Regime des beobachteten Krusten- und lithosphärischen Spannungsfeldes tragen weiter zu unserem Wissen über unterschiedliche Deformationsprozesse in der Erdkruste und Lithosphäre bei. Mit Hilfe von numerischen Modellen konnten frühere Studien die wichtigsten Kräfte identifizieren, die Spannungen in der Kruste und in der Lithosphäre erzeugen, und die auch zur Bildung von Topographie sowie zum Antrieb der lithosphärischen Platten beitragen. Sie zeigten, dass das Spannungsmuster erster Ordnung, das etwa 80% des Spannungsfeldes erklärt, aus einem Gleichgewicht der Kräfte stammt, die an der Basis der sich bewegenden lithosphärischen Platten aufgrund der konvektiven Strömung in dem darunter liegenden Mantel wirken. Das verbleibende Spannungsmuster der zweiten Ordnung ist auf laterale Dichtevariationen in der Kruste und der Lithosphäre in Regionen mit ausgeprägter Topographie und hohem Gravitationspotential zurückzuführen, wie im Himalaya und an den Mittelozeanischen Rücken. Durch die Verknüpfung der globalen Lithosphären-Dynamik mit den tiefen Mantelströmungen versucht diese Studie, den Einfluss von flachen und tiefen Dichte-Heterogenitäten auf die Plattenbewegungen, das lithosphärische Spannungsfeld und die dynamische Topographie mit dem Geoid als einer wesentlichen Randbedingung für die Mantel-Rheologie zu untersuchen. Ich verwende das globale 3D-Lithosphären-Asthenosphären-Modell SLIM3D mit viskoelasto-plastischer Rheologie, gekoppelt in 300 km Tiefe an ein spektrales Modell der Mantelströmung. Die Komplexität der Lithosphären-Asthenosphären- Komponente ermöglicht die Simulation der Power-law-Rheologie mit Kriechparametern, die sowohl Diffusions-als auch Dislokationskriechen in den obersten 300km einschließen. Zuerst untersuche ich den Einfluss der Intra-Platten-Reibung und der asthenosphärischen Viskosität auf heutige Plattenbewegungen. Bisherige Modellierungsstudien haben vorgeschlagen, dass kleine Reibungskoeffizienten ( u < 0,1, FlieSSspannung ~ 100 MPa) zu Plattentektonik in Modellen der Mantelkonvektion führen können. Hier zeigen wir, dass der Reibungsparameter, um den heutigen Plattenbewegungen und der Netto-Rotation zu entsprechen, kleiner als 0,05 sein muss. Wir können eine gute Übereinstimmung mit der Größe und Orientierung der beobachteten Plattengeschwindigkeiten (NUVEL-1A) in einem No-Net- Rotation- (NNR) Bezug system mit < 0,04 und minimaler Asthenosphärenviskosität ~ 510^19 Pas bis 10^20 Pas erreichen. Unsere Schätzungen der Netto-Rotation (NR) der Lithosphäre deuten darauf hin, dass Amplituden ~ 0:1 - 0:2 (◦/Ma), ähnlich den meisten Beobachtungs-basierten Schätzungen, mit Asthenosphären- Viskositäts-Cutoff-Werten von ~ 10^19 Pas bis 5 10^19 Pas und Reibungskoeffizient u < 0,05 erreicht werden können. Der zweite Teil der Studie untersucht weitere Einschränkungen auf flache und tiefe Mantelheterogenitäten, welche Plattenbewegungen verursachen, durch die Vorhersage des Lithosphärenspannungsfeldes und der Topographie und deren Validierung mit Beobachtungen. Lithosphärenspannungen und dynamische Topographie werden mit dem Modellaufbau und den rheologischen Parametern für vorgeschriebene Plattenbewegungen berechnet.Wir validieren unsere Ergebnisse mit der Weltspannungskarte 2016 (WSM2016) und der beobachteten Residualtopographie. Hier haben wir eine Anzahl von thermischen Dichte-Strukturen für den oberen Mantel getestet. Diejenige, die verwendet wurde, um Plattenbewegungen zu berechnen, wird als Referenz- thermische Dichte-Struktur betrachtet. Dieses Modell ist abgeleitet aus einem Wärmestrommodell, kombiniert mit einem Ozeanbodenalter-Modell. Darüber hinaus haben wir drei verschiedene thermische Dichtestrukturen abgeleitet aus globalen S-Wellengeschwindigkeits modellen verwendet, um den Einfluss von Heterogenitäten der lateralen Dichte in den oberen 300 km auf Modellvorhersagen zu zeigen. Ein großer Teil der gesamten dynamischen Kraft, die Spannungen in der Kruste / Lithosphäre erzeugt, hat ihren Ursprung im tiefen Mantel, während die Topographie weitgehend durch flache Heterogenitäten beeinflusst wird. Zum Beispiel gibt es kaum einen Unterschied zwischen den Spannungsorientierungsmustern, die mit und ohne Berücksichtigung der Heterogenitäten in der Dichtestruktur des oberen Mantels in Nordamerika, Australien und Nordafrika vorhergesagt wurden. Allerdings dominiert die Kruste in Gebieten von großer Höhe für die Spannungorientierung im Vergleich zu allen tiefen Mantelbeiträgen. Diese Studieerforschen die Empfindlichkeit aller betrachteten Oberflächen-Observablen in Bezug auf Modellparameter und gibt Einblicke über den Einfluss der Asthenosphäre und Plattengrenzen-Rheologie auf Plattenbewegung, wobei wir verschiedene thermische Dichte Strukturen zur Vorhersage von Spannungen und Topographie testen. KW - plate motions KW - plate boundary friction KW - upper mantle viscosity structure KW - lithosphere stress field KW - dynamic topography KW - lithosphere net rotation KW - upper mantle density heterogeneities KW - Plattenbewegungen KW - Reibung an Plattengrenzen KW - Viskositätsstruktur im oberen Mantel KW - lithosphärisches Spannungsfeld KW - dynamische Topographie KW - Nettorotation der Lithosphäre KW - Dichteheterogenitäten im oberen Mantel Y1 - 2017 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-407057 ER - TY - THES A1 - Bredow, Eva T1 - Geodynamic models of plume-ridge interaction T1 - Geodynamische Modelle der Interaktion von Plumes und Mittelozeanischen Rücken BT - case studies of the Réunion, Iceland and Kerguelen mantle plumes BT - Fallstudien der Réunion-, Island- und Kerguelen-Mantleplumes N2 - According to the classical plume hypothesis, mantle plumes are localized upwellings of hot, buoyant material in the Earth’s mantle. They have a typical mushroom shape, consisting of a large plume head, which is associated with the formation of voluminous flood basalts (a Large Igneous Province) and a narrow plume tail, which generates a linear, age-progressive chain of volcanic edifices (a hotspot track) as the tectonic plate migrates over the relatively stationary plume. Both plume heads and tails reshape large areas of the Earth’s surface over many tens of millions of years. However, not every plume has left an exemplary record that supports the classical hypothesis. The main objective of this thesis is therefore to study how specific hotspots have created the crustal thickness pattern attributed to their volcanic activities. Using regional geodynamic models, the main chapters of this thesis address the challenge of deciphering the three individual (and increasingly complex) Réunion, Iceland, and Kerguelen hotspot histories, especially focussing on the interactions between the respective plume and nearby spreading ridges. For this purpose, the mantle convection code ASPECT is used to set up three-dimensional numerical models, which consider the specific local surroundings of each plume by prescribing time-dependent boundary conditions for temperature and mantle flow. Combining reconstructed plate boundaries and plate motions, large-scale global flow velocities and an inhomogeneous lithosphere thickness distribution together with a dehydration rheology represents a novel setup for regional convection models. The model results show the crustal thickness pattern produced by the plume, which is compared to present-day topographic structures, crustal thickness estimates and age determinations of volcanic provinces associated with hotspot activity. Altogether, the model results agree well with surface observations. Moreover, the dynamic development of the plumes in the models provide explanations for the generation of smaller, yet characteristic volcanic features that were previously unexplained. Considering the present-day state of a model as a prediction for the current temperature distribution in the mantle, it cannot only be compared to observations on the surface, but also to structures in the Earth’s interior as imaged by seismic tomography. More precisely, in the case of the Réunion hotspot, the model demonstrates how the distinctive gap between the Maldives and Chagos is generated due to the combination of the ridge geometry and plume-ridge interaction. Further, the Rodrigues Ridge is formed as the surface expression of a long-distance sublithospheric flow channel between the upwelling plume and the closest ridge segment, confirming the long-standing hypothesis of Morgan (1978) for the first time in a dynamic context. The Réunion plume has been studied in connection with the seismological RHUM-RUM project, which has recently provided new seismic tomography images that yield an excellent match with the geodynamic model. Regarding the Iceland plume, the numerical model shows how plume material may have accumulated in an east-west trending corridor of thin lithosphere across Greenland and resulted in simultaneous melt generation west and east of Greenland. This provides an explanation for the extremely widespread volcanic material attributed to magma production of the Iceland hotspot and demonstrates that the model setup is also able to explain more complicated hotspot histories. The Iceland model results also agree well with newly derived seismic tomographic images. The Kerguelen hotspot has an extremely complex history and previous studies concluded that the plume might be dismembered or influenced by solitary waves in its conduit to produce the reconstructed variable melt production rate. The geodynamic model, however, shows that a constant plume influx can result in a variable magma production rate if the plume interacts with nearby mid-ocean ridges. Moreover, the Ninetyeast Ridge in the model is created by on-ridge activities, while the Kerguelen plume was located beneath the Australian plate. This is also a contrast to earlier studies, which described the Ninetyeast Ridge as the result of the Indian plate passing over the plume. Furthermore, the Amsterdam-Saint Paul Plateau in the model is the result of plume material flowing from the upwelling toward the Southeast Indian Ridge, whereas previous geochemical studies attributed that volcanic province to a separate deep plume. In summary, the three case studies presented in this thesis consistently highlight the importance of plume-ridge interaction in order to reconstruct the overall volcanic hotspot record as well as specific smaller features attributed to a certain hotspot. They also demonstrate that it is not necessary to attribute highly complicated properties to a specific plume in order to account for complex observations. Thus, this thesis contributes to the general understanding of plume dynamics and extends the very specific knowledge about the Réunion, Iceland, and Kerguelen mantle plumes. N2 - Nach der klassischen Plume-Hypothese sind Mantelplumes lokalisierte Aufströme aus heißem, aufsteigenden Material im Erdmantel und haben eine typische pilzförmige Struktur. Sie bestehen aus einem großen Plume-Kopf, der mit der Bildung von voluminösen Flutbasalten (einer Magmatischen Großprovinz) assoziiert wird und einem engen Plume-Schlauch, der eine lineare Kette von Vulkanen mit aufsteigendem Alter (einen Hotspot-Track) erzeugt, indem die tektonische Platte über den relativ stationären Plume wandert. Sowohl Plume-Köpfe als auch Plume-Schläuche formen große Gebiete der Erdoberfläche über viele zehn Millionen Jahre um. Allerdings hat nicht jeder Plume mustergültige Spuren hinterlassen, die die klassische Hypothese unterstützen. Das Hauptziel dieser Arbeit ist daher zu untersuchen, wie ein spezifischer Hotspot den ihm zugeordneten Hotspot-Track erzeugt hat. Mit Hilfe regionaler geodynamischer Modelle stellen sich die Hauptkapitel dieser Arbeit der Herausforderung, die drei individuellen (und zunehmend komplexen) Geschichten des Réunion-, Island- und Kerguelen-Hotspots zu entschlüsseln, wobei insbesondere die Wechselwirkungen zwischen dem jeweiligen Plume und nahegelegenen Mittelozeanischen Rücken im Mittelpunkt stehen. Zu diesem Zweck wird der Mantelkonvektions-Code ASPECT verwendet, um dreidimensionale numerische Modelle zu erstellen, die die spezielle lokale Umgebung jedes Plumes berücksichtigen, indem zeitabhängige Randbedingungen für Temperatur und Mantelströmung vorgeschrieben werden. Die Kombination von rekonstruierten Plattengrenzen und Plattenbewegungen, großräumigen globalen Strömungsgeschwindigkeiten und einer inhomogenen Lithosphärendickenverteilung zusammen mit einer Dehydrierungs-Rheologie stellt eine neue Konfiguration für regionale Konvektionsmodelle dar. Die Modellergebnisse zeigen die vom Plume produzierte Verteilung von vulkanischem Material, die mit heutigen topographischen Strukturen, Schätzungen der Krustendicke und Altersbestimmungen vulkanischer Provinzen verglichen wird. Insgesamt stimmen die Modellergebnisse gut mit den Oberflächenbeobachtungen überein. Darüber hinaus liefert die dynamische Entwicklung der Plumes in den Modellen Erklärungen für die Erzeugung kleinerer, aber charakteristischer vulkanischer Strukturen, deren Herkunft bisher unerklärt war. Betrachtet man den heutigen Zustand eines Modells als Vorhersage für die aktuelle Temperaturverteilung im Mantel, kann man ihn nicht nur mit Beobachtungen an der Oberfläche vergleichen, sondern auch mit Strukturen im Erdinneren, wie sie durch seismische Tomographie abgebildet werden. Genauer gesagt zeigt das Modell im Falle des Réunion-Hotspots, wie die charakteristische Lücke zwischen den Malediven und Chagos aufgrund der Kombination der Geometrie des Mittelozeanischen Rückens und der Interaktion zwischen Plume und Rücken erzeugt wird. Des Weiteren wird der Rodrigues-Rücken als Oberflächenerscheinung eines sublithosphärischen Strömungskanals zwischen dem aufsteigenden Plume und dem nächstgelegenen Segment des Mittelozeanischen Rückens gebildet, was die langjährige Hypothese von Morgan (1978) zum ersten Mal in einem dynamischen Kontext bestätigt. Der Réunion-Plume wurde im Rahmen des seismo- logischen RHUM-RUM-Projektes untersucht, das kürzlich neue seismische Tomographiebilder ergeben hat, die eine exzellente Übereinstimmung mit dem geodynamischen Modell aufweisen. Was den Island-Plume betrifft, so zeigt das numerische Modell, wie sich Plume-Material in einem von Ost nach West verlaufenden Korridor dünner Lithosphäre in Grönland angesammelt haben könnte und zu einer gleichzeitigen Schmelzerzeugung westlich und östlich von Grönland geführt hat. Dies erklärt das extrem weit verbreitete vulkanische Material, das der Magmaproduktion des Island-Hotspots zugeschrieben wird, und demonstriert, dass der Modell-Aufbau auch kompliziertere Hotspot-Geschichten erklären kann. Die Ergebnisse des Island-Modells stimmen ebenfalls gut mit neu erzeugten seismischen Tomographiebildern überein. Der Kerguelen-Hotspot hat eine äußerst komplexe Geschichte und frühere Studien kamen zu dem Schluss, dass der Plume eine zerrissene Struktur oder durch einzelne Wellen im Schlauch beeinflusst sein könnte, um die rekonstruierte variable Schmelzproduktionsrate zu erzeugen. Das geodynamische Modell zeigt jedoch, dass ein konstanter Plume-Einstrom zu einer variablen Magmaproduktionsrate führen kann, wenn der Plume mit nahegelegenen mittelozeanischen Rücken interagiert. Darüber hinaus wird der Neunzig-Grad-Ost-Rücken im Modell am Mittelozeanischen Rücken erschaffen, während der Kerguelen-Plume unter der australischen Platte lag. Dies steht auch im Gegensatz zu früheren Studien, die den Neunzig-Grad-Ost-Rücken als Ergebnis der über den Plume wandernden indischen Platte beschrieben haben. Darüber hinaus ist das Amsterdam-Saint Paul-Plateau im Modell das Ergebnis von Plume-Material, das von der Aufstiegsregion in Richtung des Südostindischen Rückens fließt, wohingegen frühere geochemische Studien diese vulkanische Provinz einem separaten tiefen Plume zugeschrieben haben. Zusammenfassend verdeutlichen die drei in dieser Arbeit präsentierten Fallstudien die Bedeutung der Interaktion zwischen Plume und Mittelozeanischen Rücken für die Rekonstruktion der Verteilung des gesamten vom Hotspot erzeugten vulkanischen Materials sowie von spezifischen kleineren Strukturen, die einem bestimmten Hotspot zugeordnet sind. Es wird auch gezeigt, dass es nicht notwendig ist, einem bestimmten Plume hochkomplizierte Eigenschaften zuzuschreiben, um komplexe Beobachtungen zu erklären. Somit trägt diese Arbeit zum allgemeinen Verständnis der Dynamik von Plumes bei und erweitert das sehr spezifische Wissen über die Réunion-, Island-, und Kerguelen-Mantelplumes. KW - geodynamic models KW - plume-ridge interaction KW - Réunion KW - Iceland KW - Kerguelen KW - mantle plumes KW - geodynamische Modelle KW - Plume-Rücken Interaktion KW - Réunion KW - Island KW - Kerguelen KW - Mantleplumes Y1 - 2017 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-411732 ER - TY - THES A1 - Richter, Nicole T1 - Investigating hazards and the evolution of volcanic landscapes by means of terrestrial and satellite remote sensing data and modelling Y1 - 2017 ER - TY - JOUR A1 - Fohlmeister, Jens Bernd A1 - Plessen, Birgit A1 - Dudashvili, Alexey Sergeevich A1 - Tjallingii, Rik A1 - Wolff, Christian Michael A1 - Gafurov, Abror A1 - Cheng, Hai T1 - Winter precipitation changes during the Medieval Climate Anomaly and the Little Ice Age in arid Central Asia JF - Quaternary science reviews : the international multidisciplinary research and review journal N2 - The strength of the North Atlantic Oscillation (NAO) is considered to be the main driver of climate changes over the European and western Asian continents throughout the last millennium. For example, the predominantly warm Medieval Climate Anomaly (MCA) and the following cold period of the Little Ice Age (LIA) over Europe have been associated with long-lasting phases with a positive and negative NAO index. Its climatic imprint is especially pronounced in European winter seasons. However, little is known about the influence of NAO with respect to its eastern extent over the Eurasian continent. Here we present speleothem records (PC, 8180 and Sr/Ca) from the southern rim of Fergana Basin (Central Asia) revealing annually resolved past climate variations during the last millennium. The age control of the stalagmite relies on radiocarbon dating as large amounts of detrital material inhibit accurate 230Th dating. Present-day calcification of the stalagmite is most effective during spring when the cave atmosphere and elevated water supply by snow melting and high amount of spring precipitation provide optimal conditions. Seasonal precipitation variations cause changes of the stable isotope and Sr/ Ca compositions. The simultaneous changes in these geochemical proxies, however, give also evidence for fractionation processes in the cave. By disentangling both processes, we demonstrate that the amount of winter precipitation during the MCA was generally higher than during the LIA, which is in line with climatic changes linked to the NAO index but opposite to the higher mountain records of Central Asia. Several events of strongly reduced winter precipitation are observed during the LIA in Central Asia. These dry winter events can be related to phases of a strong negative NAO index and all results reveal that winter precipitation over the central Eurasian continent is tightly linked to atmospheric NAO modes by the westerly wind systems. (C) 2017 Elsevier Ltd. All rights reserved. Y1 - 2017 U6 - https://doi.org/10.1016/j.quascirev.2017.10.026 SN - 0277-3791 VL - 178 SP - 24 EP - 36 PB - Elsevier CY - Oxford ER - TY - JOUR A1 - Sahle, Christoph J. A1 - Niskanen, Johannes A1 - Schmidt, Christian A1 - Stefanski, Johannes A1 - Gilmore, Keith A1 - Forov, Yury A1 - Jahn, Sandro A1 - Wilke, Max A1 - Sternemann, Christian T1 - Cation Hydration in Supercritical NaOH and HCl Aqueous Solutions JF - The journal of physical chemistry : B, Condensed matter, materials, surfaces, interfaces & biophysical chemistry N2 - We present a study of the local atomic environment of the oxygen atoms in the aqueous solutions of NaOH and HCl under simultaneous high-temperature and high-pressure conditions. Experimental nonresonant X-ray Raman scattering core-level spectra at the oxygen K-edge show systematic changes as a function of temperature and pressure. These systematic changes are distinct for the two different solutes and are described well by calculations within the Bethe- Salpeter formalism for snapshots from ab initio molecular dynamics simulations. The agreement between experimental and simulation results allows us to use the computations for a detailed fingerprinting analysis in an effort to elucidate the local atomic structure and hydrogen-bonding topology in these relevant solutions. We observe that both electrolytes, especially NaOH, enhance hydrogen bonding and tetrahedrality in the water structure at supercritical conditions, in particular in the vicinity of the hydration shells. This effect is accompanied with the association of the HCl and NaOH molecules at elevated temperatures. Y1 - 2017 U6 - https://doi.org/10.1021/acs.jpcb.7b09688 SN - 1520-6106 VL - 121 SP - 11383 EP - 11389 PB - American Chemical Society CY - Washington ER - TY - JOUR A1 - Schwanghart, Wolfgang A1 - Scherler, Dirk T1 - Bumps in river profiles: uncertainty assessment and smoothing using quantile regression techniques JF - Earth surface dynamics N2 - The analysis of longitudinal river profiles is an important tool for studying landscape evolution. However, characterizing river profiles based on digital elevation models (DEMs) suffers from errors and artifacts that particularly prevail along valley bottoms. The aim of this study is to characterize uncertainties that arise from the analysis of river profiles derived from different, near-globally available DEMs. We devised new algorithms quantile carving and the CRS algorithm - that rely on quantile regression to enable hydrological correction and the uncertainty quantification of river profiles. We find that globally available DEMs commonly overestimate river elevations in steep topography. The distributions of elevation errors become increasingly wider and right skewed if adjacent hillslope gradients are steep. Our analysis indicates that the AW3D DEM has the highest precision and lowest bias for the analysis of river profiles in mountainous topography. The new 12m resolution TanDEM-X DEM has a very low precision, most likely due to the combined effect of steep valley walls and the presence of water surfaces in valley bottoms. Compared to the conventional approaches of carving and filling, we find that our new approach is able to reduce the elevation bias and errors in longitudinal river profiles. Y1 - 2017 U6 - https://doi.org/10.5194/esurf-5-821-2017 SN - 2196-6311 SN - 2196-632X VL - 5 SP - 821 EP - 839 PB - Copernicus CY - Göttingen ER - TY - THES A1 - Muldashev, Iskander T1 - Modeling of the great earthquake seismic cycles T1 - Modellierung der seismischen Zyklen von Mega-Erdbeben N2 - The timing and location of the two largest earthquakes of the 21st century (Sumatra, 2004 and Tohoku 2011, events) greatly surprised the scientific community, indicating that the deformation processes that precede and follow great megathrust earthquakes remain enigmatic. During these phases before and after the earthquake a combination of multi-scale complex processes are acting simultaneously: Stresses built up by long-term tectonic motions are modified by sudden jerky deformations during earthquakes, before being restored by multiple ensuing relaxation processes. This thesis details a cross-scale thermomechanical model developed with the aim of simulating the entire subduction process from earthquake (1 minute) to million years’ time scale, excluding only rupture propagation. The model employs elasticity, non-linear transient viscous rheology, and rate-and-state friction. It generates spontaneous earthquake sequences, and, by using an adaptive time-step algorithm, recreates the deformation process as observed naturally over single and multiple seismic cycles. The model is thoroughly tested by comparing results to those from known high- resolution solutions of generic modeling setups widely used in modeling of rupture propagation. It is demonstrated, that while not modeling rupture propagation explicitly, the modeling procedure correctly recognizes the appearance of instability (earthquake) and correctly simulates the cumulative slip at a fault during great earthquake by means of a quasi-dynamic approximation. A set of 2D models is used to study the effects of non-linear transient rheology on the postseismic processes following great earthquakes. Our models predict that the viscosity in the mantle wedge drops by 3 to 4 orders of magnitude during a great earthquake with magnitude above 9. This drop in viscosity results in spatial scales and timings of the relaxation processes following the earthquakes that are significantly different to previous estimates. These models replicate centuries long seismic cycles exhibited by the greatest earthquakes (like the Great Chile 1960 Earthquake) and are consistent with the major features of postseismic surface displacements recorded after the Great Tohoku Earthquake. The 2D models are also applied to study key factors controlling maximum magnitudes of earthquakes in subduction zones. Even though methods of instrumentally observing earthquakes at subduction zones have rapidly improved in recent decades, the characteristic recurrence interval of giant earthquakes (Mw>8.5) is much larger than the currently available observational record and therefore the necessary conditions for giant earthquakes are not clear. Statistical studies have recognized the importance of the slab shape and its surface roughness, state of the strain of the upper plate and thickness of sediments filling the trenches. In this thesis we attempt to explain these observations and to identify key controlling parameters. We test a set of 2D models representing great earthquake seismic cycles at known subduction zones with various known geometries, megathrust friction coefficients, and convergence rates implemented. We found that low-angle subduction (large effect) and thick sediments in the subduction channel (smaller effect) are the fundamental necessary conditions for generating giant earthquakes, while the change of subduction velocity from 10 to 3.5 cm/yr has a lower effect. Modeling results also suggest that having thick sediments in the subduction channel causes low static friction, resulting in neutral or slightly compressive deformation in the overriding plate for low-angle subduction zones. These modeling results agree well with observations for the largest earthquakes. The model predicts the largest possible earthquakes for subduction zones of given dipping angles. The predicted maximum magnitudes exactly threshold magnitudes of all known giant earthquakes of 20th and 21st centuries. The clear limitation of most of the models developed in the thesis is their 2D nature. Development of 3D models with comparable resolution and complexity will require significant advances in numerical techniques. Nevertheless, we conducted a series of low-resolution 3D models to study the interaction between two large asperities at a subduction interface separated by an aseismic gap of varying width. The novelty of the model is that it considers behavior of the asperities during multiple seismic cycles. As expected, models show that an aseismic gap with a narrow width could not prevent rupture propagation from one asperity to another, and that rupture always crosses the entire model. When the gap becomes too wide, asperities do not interact anymore and rupture independently. However, an interesting mode of interaction was observed in the model with an intermediate width of the aseismic gap: In this model the asperities began to stably rupture in anti-phase following multiple seismic cycles. These 3D modeling results, while insightful, must be considered preliminary because of the limitations in resolution. The technique developed in this thesis for cross-scale modeling of seismic cycles can be used to study the effects of multiple seismic cycles on the long-term deformation of the upper plate. The technique can be also extended to the case of continental transform faults and for the advanced 3D modeling of specific subduction zones. This will require further development of numerical techniques and adaptation of the existing advanced highly scalable parallel codes like LAMEM and ASPECT. N2 - Zeitpunkt und Ort der zwei größten Erdbeben des 21. Jahrhunderts (Sumatra 2004 und Tohoku 2011) überraschten die wissenschaftliche Gemeinschaft, da sie darauf hindeuten, dass die einem Megathrust-Erdbeben vorangehenden und folgenden Deformationsprozesse weiterhin rästelhaft bleiben. Ein Problem ist die komplexe Art der Subduktionsprozesse auf unterschiedlichen Skalen. Spannungen werden durch langzeitliche, tektonische Bewegungen aufgebaut, von plötzlicher, ruckartiger Deformation während Erdbeben modifiziert und anschließend durch verschiedene Entspannungsprozesse wiederhergestellt. In dieser Arbeit wird ein skalen-übergreifendes thermomechanisches Modell entwickelt mit dem Ziel den vollständigen Subduktionsprozess von kleiner Skala (Minuten, z.B. Erdbeben) bis zu Millionen Jahren zu simulieren. Dabei bleibt nur das dynamische Prozess der unberücksichtigt. Das Modell nutzt Elastizität, nicht-lineare transient viskose Rheologie und „rate-and-state“ Reibungsgesetz. Es erzeugt spontane Erdbeben-Sequenzen und stellt durch das Nutzen eines adaptiven Zeitschritt Algorithmus den Deformationsprozess nach, wie er in der Natur während einzelner und mehrerer seismischer Zyklen beobachtet wird. Anhand der 2D-Modell Reihe werden die Effekte der nicht-linearen transient (viskosen) Rheologie auf postseismische Prozesse nach großen Erdbeben untersucht. Die Modelle sagen eine Verringerung der Mantelkeil-Viskosität um 3 bis 4 Größenordnungen während der großen Erdbeben (Mw > 9) vorher. Im Gegensatz zur momentanen Meinung, ergeben sich andere räumliche und zeitliche Verteilungen des Entspannungsprozesses nach großen Erdbeben. Jahrhunderte lange seismische Zyklen, wie zum Beispiel das große Erdbeben in Chile 1960, werden reproduziert und stimmen mit den Hauptmerkmalen der postseismischen Oberflächenverschiebungen überein, die nach dem großen Tohoku Erdbeben aufgezeichnet wurden. Mithilfe der 2D-Modelle werden außerdem Schlüsselfaktoren untersucht, die die maximale Magnitude von Erdbeben bestimmen. Obwohl die instrumentellen Methoden zur Beobachtung von Erdbeben in Subduktionszonen in den letzten Jahrzehnten stetig verbessert wurden, kann das Auftreten der größten Erdbeben (Mw > 8.5) und die dafür vorrauszusetzenden Bedingungen nicht genau bestimmt werden, da die charackeristische Zeit für ein Wiederauftreten deutlich größer als der Beobachtungszeitraum ist. Wir versuchen in dieser Arbeit diese Beobachtungen zu erklären und die kontrollierenden Schlüsselfaktoren zu bestimmen. Eine 2D-Modell Reihe mit großen, seismischen Erdbebenzyklen untersucht unterschiedliche Geometrien von Subduktionszonen sowie Reibungskoeffizieten an der Subduktions Platten-Grenzoberfläche und Konvergenzraten. Subduktion mit geringem Winkel (großer Effekt) und mächtige Sedimente im Subduktionskanal (kleiner Effekt) sind grundlegend notwendige Bedingungen für riesige Erdbeben, während eine Änderung des Reibungsparameters nur geringe Auswirkungen hat. Die Modellierungsergebnisse sind in viiÜbereinstimmung mit den Beobachtungen von den größten Erdbeben. Die maximale vohergesagte Magnituden liegen an der oberen Grenze alle historische Beben der 20. und 21. Jahrhunderden. Die größte Einschränkung der entwickelten Modelle ist ihre 2-dimensionale Natur. Um die Interaktion zwischen zwei großen Unebenheiten („asperities“) auf der Subduktions Platten-Grenzoberfläche, die von einer aseismischen Lücke („gap“) voneinander getrennt sind, zu untersuchen, wurde eine 3D-Modell Reihe mit geringer Auflösung durchgeführt. Neu an diesem Modell ist, dass das Verhalten der Unebenheiten während mehrerer seismischer Zyklen berücksichtigt wird. Wie erwartet zeigt das Modell, dass eine schmale, aseismische Lücke ein Propagieren von Brüchen von einer Unebenheit zur nächsten nicht verhindern kann und diese Brüche das gesamte Modell durchkreuzen. Wird die Lücke zu groß interagieren die Unebenheiten nicht mehr miteinander und brechen unabhängig voneinander. Allerdings wurde in dem Modell mit mittlerer Breite der aseismischen Lücke eine interessante Art von Interaktion beobachtet: Nach einigen seismischen Zyklen beginnen die Unebenheiten kontinuerlich und zwar in Gegen-Phasen zu brechen. Diese Ergebnisse sind andeutend, aber können aufgrund der geringen Auflösung des Models nur als vorläufig angesehen werden und erfordern weitere Bestätigung mit hoch-auflösenden Modellen. KW - earthquake modeling KW - seismic cycle modeling KW - subduction KW - numerical modeling KW - Erdbeben Modellierung KW - Modellierung des seismischen Zyklus KW - Subduktion KW - numerische Modellierung Y1 - 2017 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-398926 ER - TY - THES A1 - Hendriyana, Andri T1 - Detection and Kirchhoff-type migration of seismic events by use of a new characteristic function T1 - Detektion und Kirchhoff-Migration seismischer Ereignisse durch Verwendung einer neuen charakteristischen Funktion N2 - The classical method of seismic event localization is based on the picking of body wave arrivals, ray tracing and inversion of travel time data. Travel time picks with small uncertainties are required to produce reliable and accurate results with this kind of source localization. Hence recordings, with a low Signal-to-Noise Ratio (SNR) cannot be used in a travel time based inversion. Low SNR can be related with weak signals from distant and/or low magnitude sources as well as with a high level of ambient noise. Diffraction stacking is considered as an alternative seismic event localization method that enables also the processing of low SNR recordings by mean of stacking the amplitudes of seismograms along a travel time function. The location of seismic event and its origin time are determined based on the highest stacked amplitudes (coherency) of the image function. The method promotes an automatic processing since it does not need travel time picks as input data. However, applying diffraction stacking may require longer computation times if only limited computer resources are used. Furthermore, a simple diffraction stacking of recorded amplitudes could possibly fail to locate the seismic sources if the focal mechanism leads to complex radiation patterns which typically holds for both natural and induced seismicity. In my PhD project, I have developed a new work flow for the localization of seismic events which is based on a diffraction stacking approach. A parallelized code was implemented for the calculation of travel time tables and for the determination of an image function to reduce computation time. In order to address the effects from complex source radiation patterns, I also suggest to compute diffraction stacking from a characteristic function (CF) instead of stacking the original wave form data. A new CF, which is called in the following mAIC (modified from Akaike Information Criterion) is proposed. I demonstrate that, the performance of the mAIC does not depend on the chosen length of the analyzed time window and that both P- and S-wave onsets can be detected accurately. To avoid cross-talk between P- and S-waves due to inaccurate velocity models, I separate the P- and S-waves from the mAIC function by making use of polarization attributes. Then, eventually the final image function is represented by the largest eigenvalue as a result of the covariance analysis between P- and S-image functions. Before applying diffraction stacking, I also apply seismogram denoising by using Otsu thresholding in the time-frequency domain. Results from synthetic experiments show that the proposed diffraction stacking provides reliable results even from seismograms with low SNR=1. Tests with different presentations of the synthetic seismograms (displacement, velocity, and acceleration) shown that, acceleration seismograms deliver better results in case of high SNR, whereas displacement seismograms provide more accurate results in case of low SNR recordings. In another test, different measures (maximum amplitude, other statistical parameters) were used to determine the source location in the final image function. I found that the statistical approach is the preferred method particularly for low SNR. The work flow of my diffraction stacking method was finally applied to local earthquake data from Sumatra, Indonesia. Recordings from a temporary network of 42 stations deployed for 9 months around the Tarutung pull-apart Basin were analyzed. The seismic event locations resulting from the diffraction stacking method align along a segment of the Sumatran Fault. A more complex distribution of seismicity is imaged within and around the Tarutung Basin. Two lineaments striking N-S were found in the middle of the Tarutung Basin which support independent results from structural geology. These features are interpreted as opening fractures due to local extension. A cluster of seismic events repeatedly occurred in short time which might be related to fluid drainage since two hot springs are observed at the surface near to this cluster. N2 - Klassische seismologische Verfahren zur Lokalisierung seismischer Ereignisse basieren auf der Bestimmung der Ankunftszeiten von Raumwellenphasen, der Berechnung von Strahlwegen in Untergrundmodellen sowie der Inversion der Laufzeitdaten. Um mit dieser Methode zuverlässige und genaue Lokalisierungsergebnisse zu erhalten, werden Laufzeitdaten mit kleinen Unsicherheiten benötigt. Folgerichtig müssen Seismogramme mit sehr geringen Signal-zu-Rausch Verhältnissen (S/N) häufig verworfen werden. Geringe S/N können einerseits durch schwache Signale am Empfänger, z.B. wegen großer Entfernungen zur Quelle und/oder bei Quellen mit kleiner Magnitude, und andererseits durch einen hohen Rauschpegel verursacht werden. Eine alternative Methode zur Herdlokalisierung ist die sogenannte Diffraktions-Stapel-ung. Hierbei werden die Amplituden der aufgezeichneten Wellenformen entlang von vorhergesagten Laufzeitfunktionen aufgestapelt. Durch konstruktive Aufsummation können auch Signale von Seismogrammen mit geringem S/N zur Lokalisierung beitragen. Als Teil des Verfahrens wird eine sogenannte Image-Funktion berechnet, deren maximale Amplitude (Kohärenz) mit dem Ort und der Zeit des Bebenherdes verknüpft ist. Die Methodik ist für eine Implementation von automatisierten Überwachungssystemen geeignet. Von Nachteil ist der relative hohe Rechenaufwand. Außerdem müssen bei der Diffraktions-Stapelung die komplizierten Abstrahlcharakteristika im Quellbereich und deren Auswirkungen auf die Signale an verschiedenen Empfängern im Unterschied zur Laufzeit-Inversion mit berücksichtigt werden. In meiner Arbeit habe ich eine neue Methodik zur Lokalisierung von Bebenherden unter Verwendung einer Diffraktions-Stapelung entwickelt. Zunächst werden Laufzeiten (Green’s Funktionen) für potentielle Herdlokationen mit Hilfe eines parallelisierten Algorithmus berechnet. Eine erste Vorbearbeitung der Seismogramme mit der Otsu-Threshold-ing Methode im Zeit-Frequenz-Bereich dient zur Unterdrückung von nicht-stationären Rauschanteilen. Anschliessend wird eine neu entwickelte charakteristische Funktion (CF) berechnet, um P- und S-Welleneinsätze in den gefilterten Daten noch stärker hervorzuheben. Die vorgeschlagene CF basiert auf einer modifizierten Version des Akaike Kriteriums. Die neue CF liefert stabile Resultate, die im Unterschied zum klassischen Akaike-Kriterium nicht von der subjektiv festzulegenden Länge des Analysefensters abhängig sind. Die Verwendung der CF ist darüber hinaus entscheidend, um den unerwünschten Einfluss der Abstrahlcharakteristik auf die gemessenen Amplituden bei der Diffraktions-Stapelung zu eliminieren. Eine finale Image-Funktion wird mit Hilfe einer Kovarianzmatrix-Analyse von P- und S- Image-Funktionen bestimmt, um daraus schließlich die Herdlokation zu ermitteln. Das neue Verfahren wird an Hand von synthetischen Daten getestet. Zuverlässige und genaue Resultate konnten selbst bei sehr geringen S/N von 1 erzielt werden. Tests mit verschiedenen Seismogramm-Varianten (Verschiebung, Geschwindigkeit, Beschleunigung) ergaben, dass bei hohem S/N Beschleunigungs-Seismogramme und bei sehr niedrigen S/N Verschiebungs-Seismogramme die besten Ergebnisse lieferten. Schliesslich wurde das Verfahren auf Daten aus einer Lokalbebenuntersuchung auf Sumatra (Indonesien) angewendet. Über einen Zeitraum von 9 Monaten wurde mit einem Netzwerk aus 42 Stationen die Seismizität im Bereich des Tarutung-Beckens an der Sumatra-Störung (SF) erfasst. Die Methode bildete hierbei ein lineares Segment der SF ab. Im Tarutung-Becken wurde eine komplexere Bebenverteilung abgeleitet. Ein Vergleich mit strukturgeologischen Daten liefert Rückschlüsse auf das tektonische und geothermische Regime im Untersuchungsgebiet. KW - time-series analysis KW - inverse theory KW - earthquake source observations KW - seismicity and tectonics KW - wave scattering and diffraction KW - body waves KW - computational seismology KW - Zeitreihenanalyse KW - Inversions-Theorie KW - Beobachtung von Erdbebenquellen KW - Seismizität und Tektonik KW - Wellenbrechung und Diffraktion KW - Raumwellen KW - computergestützte Seismologie Y1 - 2017 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-398879 ER - TY - THES A1 - Ziegler, Moritz O. T1 - The 3D in-situ stress field and its changes in geothermal reservoirs T1 - Das 3D in-situ Spannungsfeld und seine Änderungen in Geothermiereservoiren N2 - Information on the contemporary in-situ stress state of the earth’s crust is essential for geotechnical applications and physics-based seismic hazard assessment. Yet, stress data records for a data point are incomplete and their availability is usually not dense enough to allow conclusive statements. This demands a thorough examination of the in-situ stress field which is achieved by 3D geomechanicalnumerical models. However, the models spatial resolution is limited and the resulting local stress state is subject to large uncertainties that confine the significance of the findings. In addition, temporal variations of the in-situ stress field are naturally or anthropogenically induced. In my thesis I address these challenges in three manuscripts that investigate (1) the current crustal stress field orientation, (2) the 3D geomechanical-numerical modelling of the in-situ stress state, and (3) the phenomenon of injection induced temporal stress tensor rotations. In the first manuscript I present the first comprehensive stress data compilation of Iceland with 495 data records. Therefore, I analysed image logs from 57 boreholes in Iceland for indicators of the orientation of the maximum horizontal stress component. The study is the first stress survey from different kinds of stress indicators in a geologically very young and tectonically active area of an onshore spreading ridge. It reveals a distinct stress field with a depth independent stress orientation even very close to the spreading centre. In the second manuscript I present a calibrated 3D geomechanical-numerical modelling approach of the in-situ stress state of the Bavarian Molasse Basin that investigates the regional (70x70x10km³) and local (10x10x10km³) stress state. To link these two models I develop a multi-stage modelling approach that provides a reliable and efficient method to derive from the larger scale model initial and boundary conditions for the smaller scale model. Furthermore, I quantify the uncertainties in the models results which are inherent to geomechanical-numerical modelling in general and the multi-stage approach in particular. I show that the significance of the models results is mainly reduced due to the uncertainties in the material properties and the low number of available stress magnitude data records for calibration. In the third manuscript I investigate the phenomenon of injection induced temporal stress tensor rotation and its controlling factors. I conduct a sensitivity study with a 3D generic thermo-hydro-mechanical model. I show that the key control factors for the stress tensor rotation are the permeability as the decisive factor, the injection rate, and the initial differential stress. In particular for enhanced geothermal systems with a low permeability large rotations of the stress tensor are indicated. According to these findings the estimation of the initial differential stress in a reservoir is possible provided the permeability is known and the angle of stress rotation is observed. I propose that the stress tensor rotations can be a key factor in terms of the potential for induced seismicity on pre-existing faults due to the reorientation of the stress field that changes the optimal orientation of faults. N2 - Kenntnis des derzeitigen in-situ Spannungszustandes der Erdkruste ist essenziell für geotechnische Anwendungen und seismische Gefährdungsabschätzungen, welche auf physikalischen Beobachtungen basieren. Jedoch sind die Spannungsinformationen jedes Datenpunktes unvollständig und die Menge an vorhandenen Datenpunkten ist normalerweise nicht groß genug, um schlüssige Ergebnisse zu erzielen. Daher ist eine eingehende Untersuchung des in-situ Spannungsfeldes, welche durch 3D geomechanisch-numerische Modellierung geleistet wird, erforderlich. Jedoch ist die räumliche Auflösung der Modelle begrenzt und der resultierende Spannungszustand ist großen Unsicherheiten unterworfen, welche die Aussagekraft der Ergebnisse beschränken. Zusätzlich gibt es zeitliche Änderungen des Spannungsfeldes, welche durch natürliche Prozesse bedingt oder menschengemacht sind. In meiner Dissertation behandle ich diese Herausforderungen in drei Manuskripten, welche (1) die Orientierung des derzeitigen Spannungszustandes, (2) die 3D geomechanisch-numerische Modellierung des in-situ Spannungszustandes und (3) das Phänomen injektionsinduzierter zeitlicher Rotationen des Spannungstensors zum Thema haben. In dem ersten Manuskript präsentiere ich die erste umfassende Spannungsdatensammlung von Island mit insgesamt 495 Einträgen. Dafür habe ich Bilddatenlogs aus 57 Bohrlöchern in Island auf Indikatoren der maximalen horizontalen Spannungsorientierung hin untersucht. Diese Studie ist die erste ganzheitliche Spannungsuntersuchung, welche sich auf verschiedene Indikatoren der Spannungsorientierung stützt und in einem geologisch sehr jungen und tektonisch aktiven Gebiet auf einem Mittelozeanischen Rücken an Land liegt. Es zeigt sich, dass selbst sehr nahe an der Plattengrenze eine tiefenunabhängige, eindeutige Spannungsorientierung existiert. In dem zweiten Manuskript präsentiere ich einen kalibrierten 3D geomechanisch-numerischen Modellierungsansatz des in-situ Spannungszustandes des bayrischen Molassebeckens welches den regionalen (70x70x10km³) und den lokalen (10x10x10km³) Spannungszustand untersucht. Um diese zwei Modelle zu verbinden, habe ich ein mehrstufigen Modellansatz entworfen, welcher eine zuverlässige und effiziente Methode darstellt um Randbedingungen und Initialbedingungen für das kleinere Modell aus dem größeren Modell abzuleiten. Des Weiteren quantifiziere ich die Unsicherheiten in den Modellergebnissen, welche im Allgemeinen durch geomechanisch-numerische Modellierung und im Speziellen durch den Mehrstufenansatz entstehen. Ich zeige, dass die Signifikanz der Modellergebnisse hauptsächlich durch die Unsicherheiten in den Materialeigenschaften sowie der geringen Anzahl vorhandener Spannungsmagnitudendaten zur Kalibrierung reduziert wird. In dem dritten Manuskript untersuche ich das Phänomen injektionsinduzierter zeitlicher Rotationen des Spannungstensors und deren kontrollierende Parameter. Ich führe eine Sensitivitätsanalyse mit einem generischen 3D thermo-hydro-mechanischen Modell durch. Darin zeige ich, dass die Schlüsselparameter, welche die Rotationen des Spannungstensors kontrollieren, die Permeabilität des Reservoirgesteins als der entscheidende Faktor, die Injektionsrate und die initiale Differenzspannung sind. Insbesondere für geothermische Systeme nach dem Hot-Dry-Rock-Verfahren mit einer geringen Permeabilität weisen die Ergebnisse auf große Rotationen des Spannungstensors hin. Gemäß diesen Ergebnissen kann die initiale Differenzspannung in einem Reservoir abgeschätzt werden, sollte die Permeabilität bekannt sein und der Winkel der Spannungsrotation beobachtet werden. Ich schlage vor, dass Spannungsrotationen ein Schlüsselfaktor in Bezug auf das Potenzial für induzierte Seismizität sind, welche auf prä-existierenden Störungen entsteht, die durch die Reorientierung des Spannungsfeldes optimal orientiert werden. KW - stress KW - stress changes KW - induced seismicity KW - geothermal KW - geomechanical modelling KW - Spannung KW - Spannungsänderungen KW - induzierte Seismizität KW - Geothermie KW - geomechanische Modellierung Y1 - 2017 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-403838 ER - TY - JOUR A1 - Boessenkool, Berry A1 - Brüger, Gerd A1 - Heistermann, Maik T1 - Effects of sample size on estimation of rainfall extremes at high temperatures JF - Natural hazards and earth system sciences N2 - High precipitation quantiles tend to rise with temperature, following the so-called Clausius–Clapeyron (CC) scaling. It is often reported that the CC-scaling relation breaks down and even reverts for very high temperatures. In our study, we investigate this reversal using observational climate data from 142 stations across Germany. One of the suggested meteorological explanations for the breakdown is limited moisture supply. Here we argue that, instead, it could simply originate from undersampling. As rainfall frequency generally decreases with higher temperatures, rainfall intensities as dictated by CC scaling are less likely to be recorded than for moderate temperatures. Empirical quantiles are conventionally estimated from order statistics via various forms of plotting position formulas. They have in common that their largest representable return period is given by the sample size. In small samples, high quantiles are underestimated accordingly. The small-sample effect is weaker, or disappears completely, when using parametric quantile estimates from a generalized Pareto distribution (GPD) fitted with L moments. For those, we obtain quantiles of rainfall intensities that continue to rise with temperature. Y1 - 2017 U6 - https://doi.org/10.5194/nhess-17-1623-2017 SN - 1561-8633 VL - 17 IS - 9 SP - 1623 EP - 1629 PB - Copernicus CY - Göttingen ER - TY - GEN A1 - Boessenkool, Berry A1 - Brüger, Gerd A1 - Heistermann, Maik T1 - Effects of sample size on estimation of rainfall extremes at high temperatures N2 - High precipitation quantiles tend to rise with temperature, following the so-called Clausius–Clapeyron (CC) scaling. It is often reported that the CC-scaling relation breaks down and even reverts for very high temperatures. In our study, we investigate this reversal using observational climate data from 142 stations across Germany. One of the suggested meteorological explanations for the breakdown is limited moisture supply. Here we argue that, instead, it could simply originate from undersampling. As rainfall frequency generally decreases with higher temperatures, rainfall intensities as dictated by CC scaling are less likely to be recorded than for moderate temperatures. Empirical quantiles are conventionally estimated from order statistics via various forms of plotting position formulas. They have in common that their largest representable return period is given by the sample size. In small samples, high quantiles are underestimated accordingly. The small-sample effect is weaker, or disappears completely, when using parametric quantile estimates from a generalized Pareto distribution (GPD) fitted with L moments. For those, we obtain quantiles of rainfall intensities that continue to rise with temperature. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 396 Y1 - 2017 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-403897 ER - TY - THES A1 - Wolf, Julia T1 - Schadenserkennung in Beton durch Überwachung mit eingebetteten Ultraschallprüfköpfen T1 - Monitoring with embedded ultrasound sensors to detect damage in concrete N2 - Die zerstörungsfreien Prüfungen von Bauwerken mit Hilfe von Ultraschallmessverfahren haben in den letzten Jahren an Bedeutung gewonnen. Durch Ultraschallmessungen können die Geometrien von Bauteilen bestimmt sowie von außen nicht sichtbare Fehler wie Delaminationen und Kiesnester erkannt werden. Mit neuartigen, in das Betonbauteil eingebetteten Ultraschallprüfköpfen sollen nun Bauwerke dauerhaft auf Veränderungen überprüft werden. Dazu werden Ultraschallsignale direkt im Inneren eines Bauteils erzeugt, was die Möglichkeiten der herkömmlichen Methoden der Bauwerksüberwachung wesentlich erweitert. Ein Ultraschallverfahren könnte mit eingebetteten Prüfköpfen ein Betonbauteil kontinuierlich integral überwachen und damit auch stetig fortschreitende Gefügeänderungen, wie beispielsweise Mikrorisse, registrieren. Sicherheitsrelevante Bauteile, die nach dem Einbau für Messungen unzugänglich oder mittels Ultraschall, beispielsweise durch zusätzliche Beschichtungen der Oberfläche, nicht prüfbar sind, lassen sich mit eingebetteten Prüfköpfen überwachen. An bereits vorhandenen Bauwerken können die Ultraschallprüfköpfe mithilfe von Bohrlöchern und speziellem Verpressmörtel auch nachträglich in das Bauteil integriert werden. Für Fertigbauteile bieten sich eingebettete Prüfköpfe zur Herstellungskontrolle sowie zur Überwachung der Baudurchführung als Werkzeug der Qualitätssicherung an. Auch die schnelle Schadensanalyse eines Bauwerks nach Naturkatastrophen, wie beispielsweise einem Erdbeben oder einer Flut, ist denkbar. Durch die gute Ankopplung ermöglichen diese neuartigen Prüfköpfe den Einsatz von empfindlichen Auswertungsmethoden, wie die Kreuzkorrelation, die Coda-Wellen-Interferometrie oder die Amplitudenauswertung, für die Signalanalyse. Bei regelmäßigen Messungen können somit sich anbahnende Schäden eines Bauwerks frühzeitig erkannt werden. Da die Schädigung eines Bauwerks keine direkt messbare Größe darstellt, erfordert eine eindeutige Schadenserkennung in der Regel die Messung mehrerer physikalischer Größen die geeignet verknüpft werden. Physikalische Größen können sein: Ultraschalllaufzeit, Amplitude des Ultraschallsignals und Umgebungstemperatur. Dazu müssen Korrelationen zwischen dem Zustand des Bauwerks, den Umgebungsbedingungen und den Parametern des gemessenen Ultraschallsignals untersucht werden. In dieser Arbeit werden die neuartigen Prüfköpfe vorgestellt. Es wird beschrieben, dass sie sich, sowohl in bereits errichtete Betonbauwerke als auch in der Konstruktion befindliche, einbauen lassen. Experimentell wird gezeigt, dass die Prüfköpfe in mehreren Ebenen eingebettet sein können da ihre Abstrahlcharakteristik im Beton nahezu ungerichtet ist. Die Mittenfrequenz von rund 62 kHz ermöglicht Abstände, je nach Betonart und SRV, von mindestens 3 m zwischen Prüfköpfen die als Sender und Empfänger arbeiten. Die Empfindlichkeit der eingebetteten Prüfköpfe gegenüber Veränderungen im Beton wird an Hand von zwei Laborexperimenten gezeigt, einem Drei-Punkt-Biegeversuch und einem Versuch zur Erzeugung von Frost-Tau-Wechsel Schäden. Die Ergebnisse werden mit anderen zerstörungsfreien Prüfverfahren verglichen. Es zeigt sich, dass die Prüfköpfe durch die Anwendung empfindlicher Auswertemethoden, auftretende Risse im Beton detektieren, bevor diese eine Gefahr für das Bauwerk darstellen. Abschließend werden Beispiele von Installation der neuartigen Ultraschallprüfköpfe in realen Bauteilen, zwei Brücken und einem Fundament, gezeigt und basierend auf dort gewonnenen ersten Erfahrungen ein Konzept für die Umsetzung einer Langzeitüberwachung aufgestellt. N2 - The non-destructive testing of concrete structures with the ultrasound method has become increasingly important in recent years. With the ultrasound technique the geometry of concrete elements can be determined and defects can be detected which are not visible on the surface, such as delaminations and honeycombs. New ultrasound sensors were developed to monitor changes in concrete structures continuously and permanently. Those ultrasound sensors will be embedded into the concrete to transmit and receive ultrasound waves within the structure. This allows a new interpretation of the condition of a structure. The use of the embedded sensors expands the options of the traditional monitoring methods. The ultrasonic technique could monitor a voluminous part of a concrete structure continuously and integral with just a few strategically placed embedded ultrasound sensors and thus register small changes in the concretes texture. Vital parts of concrete structures which are inaccessible for the ultrasonic method after construction can be monitored with embedded sensors. Inaccessibility could be caused by a surface layered with a medium reflecting or absorbing the ultrasonic wave or by to much steel obstruct"-ing the waves path. The sensors can be embedded into existing structures using boreholes and grouting mortar or installed during construction and can thus serve as a tool for quality control. The quick damage evaluation of a construction after a natural disaster such as an earthquake or a flood, is conceivable as well. As the contact between the embedded sensors and the surrounding concrete is assumed as constant over a long time, highly sensitive signal evaluation tools, such as the cross correlation between signals, the Coda Wave Interferometry and the amplitude evaluation, can be used. Therefore, with regular measurements, damage in a construction can be detected at an early stage. But, the damage of a structure can not be measured directly. A distinct damage detection needs a quantity of measured parameters, such as time of flight and amplitude of the ultrasonic wave as well as temperature, which need to be linked to each other. To achieve this, correlations between the state of the concrete construction and those parameters of the measured ultrasonic signal must be investigated. In this work the newly developed ultrasound sensors are introduced. Their installation into a concrete structure is described. The sensors sensitivity to small changes in the concrete is investigated and compared to other Non Destructive Testing (NDT) methods. The highly sensitive signal evaluation tools proof to be particularly advantageous when using embedded sensors. Installations of embedded ultrasound sensors for long time monitoring of real constructions are presented. Based on the gained experience with those installations a concept is presented for the set up of a long time monitoring system. KW - Ultraschall KW - Beton KW - Überwachung KW - Prüfköpfe KW - Temperatur KW - Frost-Tau-Wechsel KW - Schaden KW - Riss KW - ultrasound KW - concrete KW - monitoring KW - sensors KW - temperature KW - Freeze-Thaw-Cycles KW - damage KW - crack Y1 - 2017 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-397363 ER - TY - GEN A1 - Malinowski, Radosław A1 - Groom, Geoff A1 - Schwanghart, Wolfgang A1 - Heckrath, Goswin T1 - Detection and delineation of localized flooding from WorldView-2 multispectral data N2 - Remote sensing technology serves as a powerful tool for analyzing geospatial characteristics of flood inundation events at various scales. However, the performance of remote sensing methods depends heavily on the flood characteristics and landscape settings. Difficulties might be encountered in mapping the extent of localized flooding with shallow water on riverine floodplain areas, where patches of herbaceous vegetation are interspersed with open water surfaces. To address the difficulties in mapping inundation on areas with complex water and vegetation compositions, a high spatial resolution dataset has to be used to reduce the problem of mixed pixels. The main objective of our study was to investigate the possibilities of using a single date WorldView-2 image of very high spatial resolution and supporting data to analyze spatial patterns of localized flooding on a riverine floodplain. We used a decision tree algorithm with various combinations of input variables including spectral bands of the WorldView-2 image, selected spectral indices dedicated to mapping water surfaces and vegetation, and topographic data. The overall accuracies of the twelve flood extent maps derived with the decision tree method and performed on both pixels and image objects ranged between 77% and 95%. The highest mapping overall accuracy was achieved with a method that utilized all available input data and the object-based image analysis. Our study demonstrates the possibility of using single date WorldView-2 data for analyzing flooding events at high spatial detail despite the absence of spectral bands from the short-waveform region that are frequently used in water related studies. Our study also highlights the importance of topographic data in inundation analyses. The greatest difficulties were met in mapping water surfaces under dense canopy herbaceous vegetation, due to limited water surface exposure and the dominance of vegetation reflectance. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 348 KW - decision tree KW - floodplain KW - inundation KW - localized flooding KW - object-based image analysis KW - wetlands KW - WorldView-2 Y1 - 2017 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-400149 ER - TY - GEN A1 - Mielke, Christian A1 - Rogass, Christian A1 - Boesche, Nina A1 - Segl, Karl A1 - Altenberger, Uwe T1 - EnGeoMAP 2.0 BT - automated hyperspectral mineral identification for the German EnMAP space mission N2 - Algorithms for a rapid analysis of hyperspectral data are becoming more and more important with planned next generation spaceborne hyperspectral missions such as the Environmental Mapping and Analysis Program (EnMAP) and the Japanese Hyperspectral Imager Suite (HISUI), together with an ever growing pool of hyperspectral airborne data. The here presented EnGeoMAP 2.0 algorithm is an automated system for material characterization from imaging spectroscopy data, which builds on the theoretical framework of the Tetracorder and MICA (Material Identification and Characterization Algorithm) of the United States Geological Survey and of EnGeoMAP 1.0 from 2013. EnGeoMAP 2.0 includes automated absorption feature extraction, spatio-spectral gradient calculation and mineral anomaly detection. The usage of EnGeoMAP 2.0 is demonstrated at the mineral deposit sites of Rodalquilar (SE-Spain) and Haib River (S-Namibia) using HyMAP and simulated EnMAP data. Results from Hyperion data are presented as supplementary information. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 365 KW - EnMAP KW - Hyperion KW - EnGeoMAP 2.0 KW - mineral mapping KW - imaging spectroscopy Y1 - 2017 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-400650 ER - TY - GEN A1 - Bösche, Nina Kristine A1 - Rogass, Christian A1 - Lubitz, Christin A1 - Brell, Maximilian A1 - Herrmann, Sabrina A1 - Mielke, Christian A1 - Tonn, Sabine A1 - Appelt, Oona A1 - Altenberger, Uwe A1 - Kaufmann, Hermann T1 - Hyperspectral REE (Rare Earth Element) mapping of outcrops BT - applications for neodymium detection N2 - In this study, an in situ application for identifying neodymium (Nd) enriched surface materials that uses multitemporal hyperspectral images is presented (HySpex sensor). Because of the narrow shape and shallow absorption depth of the neodymium absorption feature, a method was developed for enhancing and extracting the necessary information for neodymium from image spectra, even under illumination conditions that are not optimal. For this purpose, the two following approaches were developed: (1) reducing noise and analyzing changing illumination conditions by averaging multitemporal image scenes and (2) enhancing the depth of the desired absorption band by deconvolving every image spectrum with a Gaussian curve while the rest of the spectrum remains unchanged (Richardson-Lucy deconvolution). To evaluate these findings, nine field samples from the Fen complex in Norway were analyzed using handheld X-ray fluorescence devices and by conducting detailed laboratory-based geochemical rare earth element determinations. The result is a qualitative outcrop map that highlights zones that are enriched in neodymium. To reduce the influences of non-optimal illumination, particularly at the studied site, a minimum of seven single acquisitions is required. Sharpening the neodymium absorption band allows for robust mapping, even at the outer zones of enrichment. From the geochemical investigations, we found that iron oxides decrease the applicability of the method. However, iron-related absorption bands can be used as secondary indicators for sulfidic ore zones that are mainly enriched with rare earth elements. In summary, we found that hyperspectral spectroscopy is a noninvasive, fast and cost-saving method for determining neodymium at outcrop surfaces T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 350 KW - rare earth elements KW - imaging spectroscopy KW - neodymium KW - hyperspectral KW - HySpex KW - remote sensing KW - Fen complex Y1 - 2017 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-400171 ER -