TY - JOUR A1 - Agada, S. A1 - Chen, F. A1 - Geiger, S. A1 - Toigulova, G. A1 - Agar, Susan M. A1 - Shekhar, R. A1 - Benson, Gregory S. A1 - Hehmeyer, O. A1 - Amour, Frédéric A1 - Mutti, Maria A1 - Christ, Nicolas A1 - Immenhauser, A. T1 - Numerical simulation of fluid-flow processes in a 3D high-resolution carbonate reservoir analogue JF - Petroleum geoscience N2 - A high-resolution three-dimensional (3D) outcrop model of a Jurassic carbonate ramp was used in order to perform a series of detailed and systematic flow simulations. The aim of this study was to test the impact of small- and large-scale geological features on reservoir performance and oil recovery. The digital outcrop model contains a wide range of sedimentological, diagenetic and structural features, including discontinuity surfaces, shoal bodies, mud mounds, oyster bioherms and fractures. Flow simulations are performed for numerical well testing and secondary oil recovery. Numerical well testing enables synthetic but systematic pressure responses to be generated for different geological features observed in the outcrops. This allows us to assess and rank the relative impact of specific geological features on reservoir performance. The outcome documents that, owing to the realistic representation of matrix heterogeneity, most diagenetic and structural features cannot be linked to a unique pressure signature. Instead, reservoir performance is controlled by subseismic faults and oyster bioherms acting as thief zones. Numerical simulations of secondary recovery processes reveal strong channelling of fluid flow into high-permeability layers as the primary control for oil recovery. However, appropriate reservoir-engineering solutions, such as optimizing well placement and injection fluid, can reduce channelling and increase oil recovery. Y1 - 2014 U6 - https://doi.org/10.1144/petgeo2012-096 SN - 1354-0793 VL - 20 IS - 1 SP - 125 EP - 142 PB - Geological Soc. Publ. House CY - Bath ER - TY - JOUR A1 - Aich, Valentin A1 - Liersch, Stefan A1 - Vetter, T. A1 - Huang, S. A1 - Tecklenburg, J. A1 - Hoffmann, P. A1 - Koch, H. A1 - Fournet, S. A1 - Krysanova, Valentina A1 - Mueller, N. A1 - Hattermann, Fred T1 - Comparing impacts of climate change on streamflow in four large African river basins JF - Hydrology and earth system sciences : HESS N2 - This study aims to compare impacts of climate change on streamflow in four large representative African river basins: the Niger, the Upper Blue Nile, the Oubangui and the Limpopo. We set up the eco-hydrological model SWIM (Soil and Water Integrated Model) for all four basins individually. The validation of the models for four basins shows results from adequate to very good, depending on the quality and availability of input and calibration data. For the climate impact assessment, we drive the model with outputs of five bias corrected Earth system models of Coupled Model Intercomparison Project Phase 5 (CMIP5) for the representative concentration pathways (RCPs) 2.6 and 8.5. This climate input is put into the context of climate trends of the whole African continent and compared to a CMIP5 ensemble of 19 models in order to test their representativeness. Subsequently, we compare the trends in mean discharges, seasonality and hydrological extremes in the 21st century. The uncertainty of results for all basins is high. Still, climate change impact is clearly visible for mean discharges but also for extremes in high and low flows. The uncertainty of the projections is the lowest in the Upper Blue Nile, where an increase in streamflow is most likely. In the Niger and the Limpopo basins, the magnitude of trends in both directions is high and has a wide range of uncertainty. In the Oubangui, impacts are the least significant. Our results confirm partly the findings of previous continental impact analyses for Africa. However, contradictory to these studies we find a tendency for increased streamflows in three of the four basins (not for the Oubangui). Guided by these results, we argue for attention to the possible risks of increasing high flows in the face of the dominant water scarcity in Africa. In conclusion, the study shows that impact intercomparisons have added value to the adaptation discussion and may be used for setting up adaptation plans in the context of a holistic approach. Y1 - 2014 U6 - https://doi.org/10.5194/hess-18-1305-2014 SN - 1027-5606 SN - 1607-7938 VL - 18 IS - 4 SP - 1305 EP - 1321 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Aich, Valentin A1 - Zimmermann, Alexander A1 - Elsenbeer, Helmut T1 - Quantification and interpretation of suspended-sediment discharge hysteresis patterns: How much data do we need? JF - Catena : an interdisciplinary journal of soil science, hydrology, geomorphology focusing on geoecology and landscape evolution N2 - Sediment-discharge hysteresis loops are frequently analyzed to facilitate the understanding of sediment transport processes. Hysteresis patterns, however, are often complex and their interpretation can be complicated. Particularly, quantifying hysteresis patterns remains a problematic issue. Moreover, it is currently unknown how much data is required for analyzing sediment-discharge hysteresis loops in a given area. These open questions and challenges motivated us to develop a new method for quantifying suspended-sediment hysteresis. Subsequently, we applied the new hysteresis index to three suspended-sediment and discharge datasets from a small tropical rainforest catchment. The datasets comprised a different number of events and sampling sites. Our analyses show three main findings: (1) datasets restricted to only few events, which is typical for rapid assessment surveys, were always sufficient to identify the dominating hysteresis pattern in our research area. Furthermore, some of these small datasets contained multiple-peak events that allowed identifying intra-event exhaustion effects and hence, limitations in sediment supply. (2) Datasets comprising complete hydrological years were particularly useful for analyzing seasonal dynamics of hysteresis. These analyses revealed an exhaustion of hysteresis on the inter-event scale which also points to a limited sediment supply. (3) Datasets comprising measurements from two consecutive gauges installed at the catchment outlet and on a slope within that catchment allowed analyzing the change of hysteresis patterns along the flowpath. On the slope, multiple-peak events showed a stronger intra-event exhaustion of hysteresis than at the catchment outlet. Furthermore, exhaustion of hysteresis on the inter-event scale was not evident on the slope but occurred at the catchment outlet. Our results indicate that even small sediment datasets can provide valuable insights into sediment transport processes of small catchments. Furthermore, our results may serve as a first guideline on what to expect from an analysis of hysteresis patterns for datasets of varying quality and quantity. (c) 2014 Elsevier B.V. All rights reserved. KW - Suspended sediment KW - Hysteresis index KW - Sediment monitoring KW - Overland flow KW - Tropical forest Y1 - 2014 U6 - https://doi.org/10.1016/j.catena.2014.06.020 SN - 0341-8162 SN - 1872-6887 VL - 122 SP - 120 EP - 129 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Alawi, Mashal A1 - Schneider, Beate A1 - Kallmeyer, Jens T1 - A procedure for separate recovery of extra- and intracellular DNA from a single marine sediment sample JF - Journal of microbiological methods N2 - Extracellular DNA (eDNA) is a ubiquitous biological compound in aquatic sediment and soil. Previous studies suggested that eDNA plays an important role in biogeochemical element cycling, horizontal gene transfer and stabilization of biofilm structures. Previous methods for eDNA extraction were either not suitable for oligotrophic sediments or only allowed quantification but no genetic analyses. Our procedure is based on cell detachment and eDNA liberation from sediment particles by sequential washing with an alkaline sodium phosphate buffer followed by a separation of cells and eDNA. The separated eDNA is then bound onto silica particles and purified, whereas the intracellular DNA from the separated cells is extracted using a commercial kit. The method provides extra- and intracellular DNA of high purity that is suitable for downstream applications like PCR. Extracellular DNA was extracted from organic-rich shallow sediment of the Baltic Sea, glacially influenced sediment of the Barents Sea and from the oligotrophic South Pacific Gyre. The eDNA concentration in these samples varied from 23 to 626 ng g(-1) wet weight sediment. A number of experiments were performed to verify each processing step. Although extraction efficiency is higher than other published methods, it is not fully quantitative. (C) 2014 Elsevier B.V. All rights reserved. KW - Extracellular DNA KW - eDNA KW - Intracellular DNA KW - South Pacific Gyre KW - Ancient DNA KW - Fossil DNA Y1 - 2014 U6 - https://doi.org/10.1016/j.mimet.2014.06.009 SN - 0167-7012 SN - 1872-8359 VL - 104 SP - 36 EP - 42 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Albrich, Sergi A1 - Frijia, Gianluca A1 - Parente, Mariano A1 - Caus, Esmeralda T1 - The evolution of the earliest representatives of the genus Orbitoides: Implications for Upper Cretaceous biostratigraphy JF - Cretaceous research N2 - The biostratigraphy of Campanian-Maastrichtian carbonate platforms is largely based on the larger foraminiferal genus Orbitoides. However, while the taxonomy and the chronostratigraphic age of the younger species of this genus are well established, there are still many controversies on the earliest species. We have restudied their morphological characters using a large collection of samples from the type-localities and from continuous sections in the southern Pyrenees. Based on these new observations, the long forgotten species O. sanctae-pelagiae is reinstated, while O. dordoniensis is considered a junior synonym. Successive populations of O. hottingeri, O. sanctae-pelagiae and O. douvillei show gradual morphological changes in time marked by an increase in the size and complexity of the macrospheric embryonal apparatus, an increase of the size of the adult specimens of both generations and the progressive appearance and development of true lateral chamberlets. The Font de les Bagasses Unit in the southern Pyrenees preserves a high-resolution archive of the evolution of the earliest Orbitoides. Strontium isotope stratigraphy indicates that the oldest species, O. hottingeri, made its first appearance in the earliest Campanian, close to the Santonian-Campanian boundary, and was replaced by O. sanctae-pelagiae at a level closely corresponding to the boundary between the Placenticeras bidorsatum and Menabites delawarensis ammonite zones. (C) 2014 Elsevier Ltd. All rights reserved. KW - Larger foraminifera KW - Biostratigraphy KW - Strontium isotope stratigraphy KW - Late cretaceous KW - Orbitoides Y1 - 2014 U6 - https://doi.org/10.1016/j.cretres.2014.04.013 SN - 0195-6671 SN - 1095-998X VL - 51 SP - 22 EP - 34 PB - Elsevier CY - London ER - TY - JOUR A1 - Alinaghi, Alireza A1 - Kruger, Frank T1 - Seismic array analysis and redetermination of depths of earthquakes in Tien-Shan: implications for strength of the crust and lithosphere JF - Geophysical journal international N2 - We have redetermined focal depths of moderate and major earthquakes with reported lower-crust and upper-mantle depths that have occurred in Tien-Shan, since the availability of broad-band array data. Records of earthquakes at global arrays have been used for identification and modelling of depth phases in order to make accurate estimation of focal depths. Our results show that half of the purportedly deep earthquakes are indeed originating from depths attributable to middle-crust and lower-crust regions. Also one exceptional event in the northern foreland of Tien-Shan in Junggar Basin is located in the upper mantle at the depth of 64 km. Such unusually deep earthquakes for intraplate continental tectonic domain are all located at the margin of Tien-Shan with its adjacent stable blocks and at least some of them have occurred where the brittle behaviour of continental rocks is not highly expected. The reverse mechanisms of all these earthquakes and their proximity to formerly subducting and later colliding and underplating stable blocks and their interactions with overlying Tien-Shan are clues to explain this extremity. KW - Earthquake source observations KW - Seismicity and tectonics KW - Body waves Y1 - 2014 U6 - https://doi.org/10.1093/gji/ggu141 SN - 0956-540X SN - 1365-246X VL - 198 IS - 2 SP - 1111 EP - 1129 PB - Oxford Univ. Press CY - Oxford ER - TY - JOUR A1 - Ballato, Paolo A1 - Strecker, Manfred T1 - Assessing tectonic and climatic causal mechanisms in foreland-basin stratal architecture: insights from the Alborz Mountains, northern Iran JF - Earth surface processes and landforms : the journal of the British Geomorphological Research Group N2 - The southern foreland basin of the Alborz Mountains of northern Iran is characterized by an approximately 7.3-km-thick sequence of Miocene sedimentary rocks, constituting three basin-wde coarsening-upward units spanning a period of 10(6)years. We assess available magnetostratigraphy, paleoclimatic reconstructions, stratal architecture, records of depositional environments, and sediment-provenance data to characterize the relationships between tectonically-generated accommodation space (A) and sediment supply (S). Our analysis allows an inversion of the stratigraphy for particular forcing mechanisms, documenting causal relationships, and providing a basis to decipher the relative contributions of tectonics and climate (inferred changes in precipitation) in controlling sediment supply to the foreland basin. Specifically, A/S>1, typical of each basal unit (17.5-16.0, 13.8-13.1 and 10.3-9.6Ma), is associated with sharp facies retrogradation and reflects substantial tectonic subsidence. Within these time intervals, arid climatic conditions, changes in sediment provenance, and accelerated exhumation in the orogen suggest that sediment supply was most likely driven by high uplift rates. Conversely, A/S<1 (13.8 and 13.8-11Ma, units 1, and 2) reflects facies progradation during a sharp decline in tectonic subsidence caused by localized intra-basinal uplift. During these time intervals, climate continued to be arid and exhumation active, suggesting that sediment supply was again controlled by tectonics. A/S<1, at 11-10.3Ma and 9-6-7.6Ma (and possibly 6.2; top of units 2 and 3), is also associated with two episodes of extensive progradation, but during wetter phases. The first episode appears to have been linked to a pulse in sediment supply driven by an increase in precipitation. The second episode reflects a balance between a climatically-induced increase in sediment supply and a reduction of subsidence through the incorporation of the proximal foreland into the orogenic wedge. This in turn caused an expansion of the catchment and a consequent further increase in sediment supply. KW - sediment supply KW - climatic and tectonic forcing KW - accommodation-space KW - sediment-supply ratio (A /S) KW - foreland-basin stratigraphy KW - Alborz Mountains Y1 - 2014 U6 - https://doi.org/10.1002/esp.3480 SN - 0197-9337 SN - 1096-9837 VL - 39 IS - 1 SP - 110 EP - 125 PB - Wiley-Blackwell CY - Hoboken ER - TY - JOUR A1 - Baroni, Gabriele A1 - Tarantola, S. T1 - A general probabilistic framework for uncertainty and global sensitivity analysis of deterministic models: A hydrological case study JF - Environmental modelling & software with environment data news N2 - The present study proposes a General Probabilistic Framework (GPF) for uncertainty and global sensitivity analysis of deterministic models in which, in addition to scalar inputs, non-scalar and correlated inputs can be considered as well. The analysis is conducted with the variance-based approach of Sobol/Saltelli where first and total sensitivity indices are estimated. The results of the framework can be used in a loop for model improvement, parameter estimation or model simplification. The framework is applied to SWAP, a 113 hydrological model for the transport of water, solutes and heat in unsaturated and saturated soils. The sources of uncertainty are grouped in five main classes: model structure (soil discretization), input (weather data), time-varying (crop) parameters, scalar parameters (soil properties) and observations (measured soil moisture). For each source of uncertainty, different realizations are created based on direct monitoring activities. Uncertainty of evapotranspiration, soil moisture in the root zone and bottom fluxes below the root zone are considered in the analysis. The results show that the sources of uncertainty are different for each output considered and it is necessary to consider multiple output variables for a proper assessment of the model. Improvements on the performance of the model can be achieved reducing the uncertainty in the observations, in the soil parameters and in the weather data. Overall, the study shows the capability of the GPF to quantify the relative contribution of the different sources of uncertainty and to identify the priorities required to improve the performance of the model. The proposed framework can be extended to a wide variety of modelling applications, also when direct measurements of model output are not available. KW - Global sensitivity analysis KW - Non-scalar input factors KW - Hydrological model KW - Multi-variables Y1 - 2014 U6 - https://doi.org/10.1016/j.envsoft.2013.09.022 SN - 1364-8152 SN - 1873-6726 VL - 51 SP - 26 EP - 34 PB - Elsevier CY - Oxford ER - TY - JOUR A1 - Basavaiah, Nathani A1 - Wiesner, M. G. A1 - Anoop, Ambili A1 - Menzel, P. A1 - Nowaczyk, Norbert R. A1 - Deenadayalan, K. A1 - Brauer, Achim A1 - Gaye, Birgit A1 - Naumann, R. A1 - Riedel, N. A1 - Stebich, M. A1 - Prasad, Sushma T1 - Physicochemical analyses of surface sediments from the Lonar Lake, central India - implications for palaeoenvironmental reconstruction JF - Fundamental and applied limnology : official journal of the International Association of Theoretical and Applied Limnology N2 - We report the results of our investigations on the catchment area, surface sediments, and hydrology of the monsoonal Lonar Lake, central India. Our results indicate that the lake is currently stratified with an anoxic bottom layer, and there is a spatial heterogeneity in the sensitivity of sediment parameters to different environmental processes. In the shallow (0-5 m) near shore oxic-suboxic environments the lithogenic and terrestrial organic content is high and spatially variable, and the organics show degradation in the oxic part. Due to aerial exposure resulting from lake level changes of at least 3m, the evaporitic carbonates are not completely preserved. In the deep water (>5 m) anoxic environment the lithogenics are uniformly distributed and the delta C-13 is an indicator not only for aquatic vs. terrestrial plants but also of lake pH and salinity. The isotopic composition of the evaporites is dependent not only on the isotopic composition of source water (monsoon rainfall and stream inflow) and evaporation, but is also influenced by proximity to the isotopically depleted stream inflow. We conclude that in the deep water environment lithogenic content, and isotopic composition of organic matter can be used for palaeoenvironmental reconstruction. KW - isotopes KW - lonar lake KW - modern surface sediments KW - magnetic parameters KW - monsoon KW - palaeoenvironmental proxies Y1 - 2014 U6 - https://doi.org/10.1127/1863-9135/2014/0515 SN - 1863-9135 VL - 184 IS - 1 SP - 51 EP - 68 PB - Schweizerbart CY - Stuttgart ER - TY - THES A1 - Bathke, Hannes T1 - An investigation of complex deformation patterns detected by using InSAR at Llaima and Tendürek volcanoes T1 - Eine Untersuchung von komplexen Erdoberflächenverformungen gemessen mit InSAR, an den Vulkanen Llaima und Tendürek N2 - Surface displacement at volcanic edifices is related to subsurface processes associated with magma movements, fluid transfers within the volcano edifice and gravity-driven deformation processes. Understanding of associated ground displacements is of importance for assessment of volcanic hazards. For example, volcanic unrest is often preceded by surface uplift, caused by magma intrusion and followed by subsidence, after the withdrawal of magma. Continuous monitoring of the surface displacement at volcanoes therefore might allow the forecasting of upcoming eruptions to some extent. In geophysics, the measured surface displacements allow the parameters of possible deformation sources to be estimated through analytical or numerical modeling. This is one way to improve the understanding of subsurface processes acting at volcanoes. Although the monitoring of volcanoes has significantly improved in the last decades (in terms of technical advancements and number of monitored volcanoes), the forecasting of volcanic eruptions remains puzzling. In this work I contribute towards the understanding of the subsurface processes at volcanoes and thus to the improvement of volcano eruption forecasting. I have investigated the displacement field of Llaima volcano in Chile and of Tendürek volcano in East Turkey by using synthetic aperture radar interferometry (InSAR). Through modeling of the deformation sources with the extracted displacement data, it was possible to gain insights into potential subsurface processes occurring at these two volcanoes that had been barely studied before. The two volcanoes, although of very different origin, composition and geometry, both show a complexity of interacting deformation sources. At Llaima volcano, the InSAR technique was difficult to apply, due to the large decorrelation of the radar signal between the acquisition of images. I developed a model-based unwrapping scheme, which allows the production of reliable displacement maps at the volcano that I used for deformation source modeling. The modeling results show significant differences in pre- and post-eruptive magmatic deformation source parameters. Therefore, I conjecture that two magma chambers exist below Llaima volcano: a post-eruptive deep one and a shallow one possibly due to the pre-eruptive ascent of magma. Similar reservoir depths at Llaima have been confirmed by independent petrologic studies. These reservoirs are interpreted to be temporally coupled. At Tendürek volcano I have found long-term subsidence of the volcanic edifice, which can be described by a large, magmatic, sill-like source that is subject to cooling contraction. The displacement data in conjunction with high-resolution optical images, however, reveal arcuate fractures at the eastern and western flank of the volcano. These are most likely the surface expressions of concentric ring-faults around the volcanic edifice that show low magnitudes of slip over a long time. This might be an alternative mechanism for the development of large caldera structures, which are so far assumed to be generated during large catastrophic collapse events. To investigate the potential subsurface geometry and relation of the two proposed interacting sources at Tendürek, a sill-like magmatic source and ring-faults, I have performed a more sophisticated numerical modeling approach. The optimum source geometries show, that the size of the sill-like source was overestimated in the simple models and that it is difficult to determine the dip angle of the ring-faults with surface displacement data only. However, considering physical and geological criteria a combination of outward-dipping reverse faults in the west and inward-dipping normal faults in the east seem to be the most likely. Consequently, the underground structure at the Tendürek volcano consists of a small, sill-like, contracting, magmatic source below the western summit crater that causes a trapdoor-like faulting along the ring-faults around the volcanic edifice. Therefore, the magmatic source and the ring-faults are also interpreted to be temporally coupled. In addition, a method for data reduction has been improved. The modeling of subsurface deformation sources requires only a relatively small number of well distributed InSAR observations at the earth’s surface. Satellite radar images, however, consist of several millions of these observations. Therefore, the large amount of data needs to be reduced by several orders of magnitude for source modeling, to save computation time and increase model flexibility. I have introduced a model-based subsampling approach in particular for heterogeneously-distributed observations. It allows a fast calculation of the data error variance-covariance matrix, also supports the modeling of time dependent displacement data and is, therefore, an alternative to existing methods. N2 - Oberflächenverschiebungen an Vulkanen können einerseits durch unterirdische Magmen- oder Fluidbewegungen oder andererseits durch Gravitation verursacht werden. So sind insbesondere vor Eruptionen oft Aufwölbungen an Vulkanen zu beobachten, verursacht durch Magmenintrusion in die Erdkruste. Nach Eruptionen hingegen sinkt das Vulkangebäude aufgrund von Magmenextrusion wieder. Kontinuierliche Messungen an Vulkanen ermöglichen es, Eruptionen teilweise bis auf wenige Tage vorherzusagen. Die gemessenen Oberflächenverschiebungen können in analytischen oder numerischen Modellierungen genutzt werden, um Parameter eines möglichen Quellprozesses abzuschätzen. Auf diese Art und Weise kann das Verständnis über die unterirdischen Prozesse, die an Vulkanen stattfinden, verbessert werden. Obwohl es in den letzten Jahrzehnten eine enorme Entwicklung und Verbesserung der Überwachung von Vulkanen gab, sind viele Vorhersagen sehr vage und ungenau. Mit dieser Arbeit möchte ich einen Beitrag zum Verständnis von unterirdischen Prozessen an Vulkanen und auf lange Sicht gesehen, zur Vorhersage von Eruptionen leisten. Ich habe die Vulkane, Llaima in Chile und Tendürek im Osten der Türkei, mit Hilfe der Interferometrie von Radardaten (InSAR) untersucht. Die somit gemessenen Verschiebungen an der Erdoberfläche ermöglichen es, durch Modellierung der möglichen Deformationsquellen, Informationen über die Untergrundstrukturen dieser beiden bisher kaum erforschten Vulkane zu bekommen. Obwohl unterschiedlich in Aufbau, Gesteinszusammensetzung und Entstehung, zeigen beide Vulkane Anzeichen dafür, dass jeweils mehrere interagierende Deformationsquellen im Untergrund existieren. Am Vulkan Llaima war es schwierig, aufgrund der starken Dekorrelation des Radarsignals zwischen den Satellitenaufnahmen, die InSAR Methode anzuwenden. Ich entwickelte eine Methode um die doppeldeutigen relativen Phasenwerte der Interferogramme modellbasiert in eindeutige relative Phasenwerte umzurechnen. Die damit erzeugten Oberflächenverschiebungskarten am Vulkan eigneten sich nun für eine anschließende Modellierung der Deformationsquelle. Die Modellierungsergebnisse zeigen signifikante Unterschiede zwischen den Parametern der präeruptiven- und posteruptiven Deformationsquellen. Demzufolge könnten zwei unterschiedliche, interagierende Magmenkammern unter Llaima existieren, eine tiefe, posteruptiv aktive Kammer und eine flache, durch den Aufstieg von Magma präeruptiv aktive Kammer. Am Vulkan Tendürek ist eine langfristige, kontinuierliche Senkung des Vulkangebäudes zu beobachten, die mit einem großen, aufgrund von Kühlung sich kontrahierenden, magmatischen Sill, erklärbar ist. Unter Hinzunahme von hochauflösenden, optischen Daten jedoch, sind bei genauerer Untersuchung bogenförmige Strukturen an der Erdoberfläche sichtbar. Diese sind Anzeichen dafür, dass Verwerfungen existieren, die das gesamte Vulkangebäude in einem elliptischen Ring umgeben. Dabei ist zu beobachten, dass die Ringstörungen über Jahrtausende, möglicherweise sogar kontinuierlich, geringe Magnituden von Versatz aufweisen. Bei langer, kontinuierlicher Aktivität über mehrere zehntausende von Jahren, könnte dies ein weiterer Mechanismus zur Entstehung von Calderastrukturen an Vulkanen darstellen, der jedoch sehr langsam verläuft. Im Gegensatz dazu ist die heutige weit verbreitete Auffassung, dass Calderen als Folge katastrophaler Einstürze von Vulkangebäuden entstehen. Um zu untersuchen welche Geometrie die vorgeschlagenen Strukturen Sill und Ringstörungen an Tendürek im Untergund haben könnten, vollführte ich eine weitaus komplexere numerische Modellierung. Diese zeigt, dass die Größe des Sills ohne Berücksichtigung der Ringstörung um ein Vielfaches überschätzt ist. Die Orientierung und Geometrie der Ringstörungen ist jedoch nicht eindeutig nur mit Oberflächenverschiebungsdaten auflösbar. Unter der Berücksichtigung von geologischen und physikalischen Gesichtspunkten sind nach Außen einfallende Aufschiebungen im Westen und nach Innen einfallende Abschiebungen im Osten die plausibelste Erklärung. Außerdem habe ich eine Methode zur Datenreduzierung entwickelt. Abhängig vom zu untersuchenden Prozess sind für die Modellierung von unterirdischen Deformationsquellen verhältnismäßig wenige gut verteilte Messpunkte an der Erdoberfläche ausreichend. Satelliten gestützte Radaraufnahmen haben jedoch oft mehrere Millionen dieser Punkte. Deshalb müssen diese riesigen Datensätze auf eine Art und Weise reduziert werden, dass keine oder nur möglichst wenige Informationen verloren gehen. Für diesen Zweck habe ich, ausgehend von einem existierenden Algorithmus, eine modellbasierte Methode zur Reduzierung von besonders heterogen verteilten Oberflächendaten entwickelt. Diese Methode ist besonders gut auf Zeitreihendatensätze anwendbar und stellt somit eine Alternative zu existierenden Algorithmen dar. KW - InSAR KW - Deformationsquellenmodellierung KW - Llaima Vulkan KW - Tendürek Vulkan KW - Ringstörungen KW - InSAR KW - deformation source modeling KW - Llaima volcano KW - Tendürek volcano KW - ring-fault Y1 - 2014 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus-70522 ER - TY - JOUR A1 - Bhatt, Kaushalendra M. T1 - Microseisms and its impact on the marine-controlled source electromagnetic signal JF - Journal of geophysical research : Solid earth N2 - The marine-controlled source electromagnetic method (mCSEM) is employed for studying the electrical characteristics and fluid contents of sedimentary reservoirs. However, the success rate of the method can be improved significantly by finding the sources of electromagnetic noise and addressing the challenge posed by them at larger offsets where the reservoir signal is often weak. I have studied the mCSEM data and reporting an electromagnetic noise. The strength of the noise is observed 1600 times stronger than the seafloor mCSEM signal at 0.1 Hz. Moreover, the noise and the transmitted mCSEM signals are found coherent in interstation recordings. These readings suggest the severity of the noise. The source investigation presuming the observed noise as an infragravity wave failed to match the response. Then, the role of microseisms is investigated. Microseism causes oscillation of the seafloor and produces electromagnetic disturbances by the dynamics of water. I have used various conditions for a proper discrimination of the noise as microseisms. This mechanism is clearly illustrated with the help of a conceptual diagram. The role of the directionality is part of the study, which is argued for having a significant role in the generation of microseisms. In this paper, a new algorithm is presented and is used for calculating the coherency. The algorithm helps in mapping the coherency value simultaneously in time and frequency domains. KW - microseisms KW - marine-controlled source electromagnetic method KW - spectrogram KW - coherency KW - Pierson-Moskowitz spectra Y1 - 2014 U6 - https://doi.org/10.1002/2014JB011024 SN - 2169-9313 SN - 2169-9356 VL - 119 IS - 12 SP - 8655 EP - 8666 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Bloethe, Jan H. A1 - Munack, Henry A1 - Korup, Oliver A1 - Fuelling, Alexander A1 - Garzanti, Eduardo A1 - Resentini, Alberto A1 - Kubik, Peter W. T1 - Late Quaternary valley infill and dissection in the Indus River, western Tibetan Plateau margin JF - Quaternary science reviews : the international multidisciplinary research and review journal N2 - The Indus, one of Earth's major rivers, drains large parts of the NW Himalaya and the Transhimalayan ranges that form part of the western Tibetan Plateau margin. In the western Himalayan syntaxis, where local topographic relief exceeds 7 km, the Indus has incised a steep bedrock gorge at rates of several mm yr(-1). Upstream, however, the upper Indus and its tributaries alternate between bedrock gorges and broad alluvial flats flanked by the Ladakh and Zanskar ranges. We review the late Quaternary valley history in this region with a focus on the confluence of the Indus and Zanskar Rivers, where vast alluvial terrace staircases and lake sediments record major episodes of aggradation and incision. New absolute dating of high-level fluvial terrace remnants using cosmogenic Be-10, optically and infrared stimulated luminescence (OSL, IRSL) indicates at least two phases of late Quaternary valley infilling. These phases commenced before similar to 200 ka and similar to 50-20 ka, judging from terrace treads stranded >150 m and similar to 30-40 m above modern river levels, respectively. Numerous stacks of lacustrine sediments that straddle the Indus River >200 km between the city of Leh and the confluence with the Shyok River share a distinct horizontal alignment. Constraints from IRSL samples of lacustrine sequences from the Leh-Spituk area reveal a protracted lake phase from >177 ka to 72 ka, locally accumulating >50-m thick deposits. In the absence of tectonic faulting, major lithological differences, and stream capture, we attribute the formation of this and other large lakes in the region to natural damming by large landslides, glaciers, and alluvial fans. The overall patchy landform age constraints from earlier studies can be reconciled by postulating a major deglacial control on sediment flux, valley infilling, and subsequent incision that has been modulated locally by backwater effects of natural damming. While comparison with Pleistocene monsoon proxies reveals no obvious correlation, a lateor post-glacial sediment pulse seems a more likely source of this widespread sedimentation that has partly buried the dissected bedrock topography. Overall, the long residence times of fluvial, alluvial and lacustrine deposits in the region (>500 ka) support previous studies, but remain striking given the dominantly steep slopes and deeply carved valleys that characterise this high-altitude mountain desert. Recalculated late Quaternary rates of fluvial bedrock incision in the Indus and Zanskar of 1.5 +/- 0.2 mm yr(-1) are at odds with the longevity of juxtaposed valley-fill deposits, unless a lack of decisive lateral fluvial erosion helps to preserve these late Pleistocene sedimentary archives. We conclude that alternating, similar to 10(4)-yr long, phases of massive infilling and incision have dominated the late Quaternary history of the Indus valley below the western Tibetan Plateau margin. (C) 2014 Elsevier Ltd. All rights reserved. KW - Himalaya KW - Indus KW - Valley fills KW - Glaciation KW - Erosion KW - Lake sediment Y1 - 2014 U6 - https://doi.org/10.1016/j.quascirev.2014.04.011 SN - 0277-3791 VL - 94 SP - 102 EP - 119 PB - Elsevier CY - Oxford ER - TY - THES A1 - Borchardt, Sven T1 - Rainfall, weathering and erosion BT - quantification of earth surface processes in Suguta Valley, northern Kenya, using multispectral and hyperspectral data Y1 - 2014 ER - TY - JOUR A1 - Bouwer, Laurens M. A1 - Papyrakis, Elissaios A1 - Poussin, Jennifer A1 - Pfurtscheller, Clemens A1 - Thieken, Annegret T1 - The costing of measures for natural hazard mitigation in Europe JF - Natural hazards review N2 - The literature on the costing of mitigation measures for reducing impacts of natural hazards is rather fragmented. This paper provides a concise overview of the current state of knowledge in Europe on the costing of mitigation measures for the reduction of natural hazard risks (droughts, floods, storms and induced coastal hazards as well as alpine hazards) and identifies knowledge gaps and related research recommendations. Furthermore, it provides a taxonomy of related mitigation options, classifying them into nine categories: (1) management plans, land-use planning, and climate adaptation; (2) hazard modification; (3) infrastructure; (4) mitigation measures (stricto sensu); (5) communication in advance of events; (6) monitoring and early warning systems; (7) emergency response and evacuation; (8) financial incentives; and (9) risk transfer (including insurance). It is found that the costing of mitigation measures in European and in other countries has almost exclusively focused on estimating direct costs. A cost assessment framework that addresses a range of costs, possibly informed by multiple stakeholders, would provide more accurate estimates and could provide better guidance to decision makers. (C) 2014 American Society of Civil Engineers. KW - Natural hazards KW - Mitigation KW - Costs KW - Adaptation KW - Risk reduction KW - Floods KW - Droughts KW - Coastal hazards KW - Alpine hazards Y1 - 2014 U6 - https://doi.org/10.1061/(ASCE)NH.1527-6996.0000133 SN - 1527-6988 SN - 1527-6996 VL - 15 IS - 4 PB - American Society of Civil Engineers CY - Reston ER - TY - JOUR A1 - Braeuer, Benjamin A1 - Asch, Günter A1 - Hofstetter, Rami A1 - Haberland, Christian A1 - Jaser, D. A1 - El-Kelani, R. A1 - Weber, Michael H. T1 - Detailed seismicity analysis revealing the dynamics of the southern Dead Sea area JF - Journal of seismology N2 - Within the framework of the international DESIRE (DEad Sea Integrated REsearch) project, a dense temporary local seismological network was operated in the southern Dead Sea area. During 18 recording months, 648 events were detected. Based on an already published tomography study clustering, focal mechanisms, statistics and the distribution of the microseismicity in relation to the velocity models from the tomography are analysed. The determined b value of 0.74 leads to a relatively high risk of large earthquakes compared to the moderate microseismic activity. The distribution of the seismicity indicates an asymmetric basin with a vertical strike-slip fault forming the eastern boundary of the basin, and an inclined western boundary, made up of strike-slip and normal faults. Furthermore, significant differences between the area north and south of the Bokek fault were observed. South of the Bokek fault, the western boundary is inactive while the entire seismicity occurs on the eastern boundary and below the basin-fill sediments. The largest events occurred here, and their focal mechanisms represent the northwards transform motion of the Arabian plate along the Dead Sea Transform. The vertical extension of the spatial and temporal cluster from February 2007 is interpreted as being related to the locking of the region around the Bokek fault. North of the Bokek fault similar seismic activity occurs on both boundaries most notably within the basin-fill sediments, displaying mainly small events with strike-slip mechanism and normal faulting in EW direction. Therefore, we suggest that the Bokek fault forms the border between the single transform fault and the pull-apart basin with two active border faults. KW - Dead Sea basin KW - Microseismicity KW - Cluster KW - Pull-apart basin KW - Asymmetric basin KW - Transform fault Y1 - 2014 U6 - https://doi.org/10.1007/s10950-014-9441-4 SN - 1383-4649 SN - 1573-157X VL - 18 IS - 4 SP - 731 EP - 748 PB - Springer CY - Dordrecht ER - TY - JOUR A1 - Bronstert, Axel A1 - de Araujo, Jose-Carlos A1 - Batalla Villanueva, Ramon J. A1 - Costa, Alexandre Cunha A1 - Delgado, José Miguel Martins A1 - Francke, Till A1 - Förster, Saskia A1 - Guentner, Andreas A1 - Lopez-Tarazon, José Andrés A1 - Mamede, George Leite A1 - Medeiros, Pedro Henrique Augusto A1 - Mueller, Eva A1 - Vericat, Damia T1 - Process-based modelling of erosion, sediment transport and reservoir siltation in mesoscale semi-arid catchments JF - Journal of soils and sediments : protection, risk assessment and remediation N2 - To support scientifically sound water management in dryland environments a modelling system has been developed for the quantitative assessment of water and sediment fluxes in catchments, transport in the river system, and retention in reservoirs. The spatial scale of interest is the mesoscale because this is the scale most relevant for management of water and land resources. This modelling system comprises process-oriented hydrological components tailored for dryland characteristics coupled with components comprising hillslope erosion, sediment transport and reservoir deposition processes. The spatial discretization is hierarchically designed according to a multi-scale concept to account for particular relevant process scales. The non-linear and partly intermittent run-off generation and sediment dynamics are dealt with by accounting for connectivity phenomena at the intersections of landscape compartments. The modelling system has been developed by means of data from nested research catchments in NE-Spain and in NE-Brazil. In the semi-arid NE of Brazil sediment retention along the topography is the main process for sediment retention at all scales, i.e. the sediment delivery is transport limited. This kind of deposition retains roughly 50 to 60 % of eroded sediment, maintaining a similar deposition proportion in all spatial scales investigated. On the other hand, the sediment retained in reservoirs is clearly related to the scale, increasing with catchment area. With increasing area, there are more reservoirs, increasing the possibility of deposition. Furthermore, the area increase also promotes an increase in flow volume, favouring the construction of larger reservoirs, which generally overflow less frequently and retain higher sediment fractions. The second example comprises a highly dynamic Mediterranean catchment in NE-Spain with nested sub-catchments and reveals the full dynamics of hydrological, erosion and deposition features. The run-off modelling performed well with only some overestimation during low-flow periods due to the neglect of water losses along the river. The simulated peaks in sediment flux are reproduced well, while low-flow sediment transport is less well captured, due to the disregard of sediment remobilization in the riverbed during low flow. This combined observation and modelling study deepened the understanding of hydro-sedimentological systems characterized by flashy run-off generation and by erosion and sediment transport pulses through the different landscape compartments. The connectivity between the different landscape compartments plays a very relevant role, regarding both the total mass of water and sediment transport and the transport time through the catchment. KW - Connectivity KW - Deposition KW - Erosion KW - Modelling KW - Sediment transfer KW - Semi-arid Y1 - 2014 U6 - https://doi.org/10.1007/s11368-014-0994-1 SN - 1439-0108 SN - 1614-7480 VL - 14 IS - 12 SP - 2001 EP - 2018 PB - Springer CY - Heidelberg ER - TY - JOUR A1 - Brosinsky, Arlena A1 - Förster, Saskia A1 - Segl, Karl A1 - Kaufmann, Hermann T1 - Spectral fingerprinting: sediment source discrimination and contribution modelling of artificial mixtures based on VNIR-SWIR spectral properties JF - Journal of soils and sediments : protection, risk assessment and remediation N2 - Knowledge of the origin of suspended sediment is important for improving our understanding of sediment dynamics and thereupon support of sustainable watershed management. An direct approach to trace the origin of sediments is the fingerprinting technique. It is based on the assumption that potential sediment sources can be discriminated and that the contribution of these sources to the sediment can be determined on the basis of distinctive characteristics (fingerprints). Recent studies indicate that visible-near-infrared (VNIR) and shortwave-infrared (SWIR) reflectance characteristics of soil may be a rapid, inexpensive alternative to traditional fingerprint properties (e.g. geochemistry or mineral magnetism). To further explore the applicability of VNIR-SWIR spectral data for sediment tracing purposes, source samples were collected in the Isabena watershed, a 445 km(2) dryland catchment in the central Spanish Pyrenees. Grab samples of the upper soil layer were collected from the main potential sediment source types along with in situ reflectance spectra. Samples were dried and sieved, and artificial mixtures of known proportions were produced for algorithm validation. Then, spectral readings of potential source and artificial mixture samples were taken in the laboratory. Colour coefficients and physically based parameters were calculated from in situ and laboratory-measured spectra. All parameters passing a number of prerequisite tests were subsequently applied in discriminant function analysis for source discrimination and mixing model analyses for source contribution assessment. The three source types (i.e. badlands, forest/grassland and an aggregation of other sources, including agricultural land, shrubland, unpaved roads and open slopes) could be reliably identified based on spectral parameters. Laboratory-measured spectral fingerprints permitted the quantification of source contribution to artificial mixtures, and introduction of source heterogeneity into the mixing model decreased accuracies for some source types. Aggregation of source types that could not be discriminated did not improve mixing model results. Despite providing similar discrimination accuracies as laboratory source parameters, in situ derived source information was found to be insufficient for contribution modelling. The laboratory mixture experiment provides valuable insights into the capabilities and limitations of spectral fingerprint properties. From this study, we conclude that combinations of spectral properties can be used for mixing model analyses of a restricted number of source groups, whereas more straightforward in situ measured source parameters do not seem suitable. However, modelling results based on laboratory parameters also need to be interpreted with care and should not rely on the estimates of mean values only but should consider uncertainty intervals as well. KW - Artificial mixture KW - Mixing model KW - Sediment fingerprinting KW - Spectroscopy Y1 - 2014 U6 - https://doi.org/10.1007/s11368-014-0925-1 SN - 1439-0108 SN - 1614-7480 VL - 14 IS - 12 SP - 1949 EP - 1964 PB - Springer CY - Heidelberg ER - TY - JOUR A1 - Brosinsky, Arlena A1 - Förster, Saskia A1 - Segl, Karl A1 - Lopez-Tarazon, José Andrés A1 - Pique, Gemma A1 - Bronstert, Axel T1 - Spectral fingerprinting: characterizing suspended sediment sources by the use of VNIR-SWIR spectral information JF - Journal of soils and sediments : protection, risk assessment and remediation N2 - Knowledge of sediment sources is a prerequisite for sustainable management practices and may furthermore improve our understanding of water and sediment fluxes. Investigations have shown that a number of characteristic soil properties can be used as "fingerprints" to trace back the sources of river sediments. Spectral properties have recently been successfully used as such characteristics in fingerprinting studies. Despite being less labour-intensive than geochemical analyses, for example, spectroscopy allows measurements of small amounts of sediment material (> 60 mg), thus enabling inexpensive analyses even of intra-event variability. The focus of this study is on the examination of spectral properties of fluvial sediment samples to detect changes in source contributions, both between and within individual flood events. Sediment samples from the following three different origins were collected in the Isabena catchment (445 km(2)) in the central Spanish Pyrenees: (1) soil samples from the main potential source areas, (2) stored fine sediment from the channel bed once each season in 2011 and (3) suspended sediment samples during four flood events in autumn 2011 and spring 2012 at the catchment outlet as well as at several subcatchment outlets. All samples were dried and measured for spectral properties in the laboratory using an ASD spectroradiometer. Colour parameters and physically based features (e.g. organic carbon, iron oxide and clay content) were calculated from the spectra. Principal component analyses (PCA) were applied to all three types of samples to determine natural clustering of samples, and a mixing model was applied to determine source contributions. We found that fine sediment stored in the river bed seems to be mainly influenced by grain size and seasonal variability, while sampling location-and thus the effect of individual tributaries or subcatchments-seem to be of minor importance. Suspended sediment sources were found to vary between, as well as within, flood events; although badlands were always the major source. Forests and grasslands contributed little (< 10 %), and other sources (not further determinable) contributed up to 40 %. The analyses further suggested that sediment sources differ among the subcatchments and that subcatchments comprising relatively large proportions of badlands contributed most to the four flood events analyzed. Spectral fingerprints provide a rapid and cost-efficient alternative to conventional fingerprint properties. However, a combination of spectral and conventional fingerprint properties could potentially permit discrimination of a larger number of source types. KW - Isabena river KW - Mixing models KW - Northeast Spain KW - Sediment fingerprinting KW - Spectroscopy KW - Suspended sediment Y1 - 2014 U6 - https://doi.org/10.1007/s11368-014-0927-z SN - 1439-0108 SN - 1614-7480 VL - 14 IS - 12 SP - 1965 EP - 1981 PB - Springer CY - Heidelberg ER - TY - JOUR A1 - Bruttel, Lisa Verena A1 - Friehe, Tim T1 - Can short-term incentives induce long-lasting cooperation? Results from a public-goods experiment JF - Journal of behavioral and experimental economics N2 - This paper investigates whether providing strong cooperation incentives only at the outset of a group interaction spills over to later periods to ensure cooperation in the long run. We study a repeated linear public-good game with punishment opportunities and a parameter change after the first ten (of twenty) rounds. Our data shows that cooperation among subjects who had experienced a higher marginal return on public-good contributions or low punishment costs in rounds 1-10 rapidly deteriorated in rounds 11-20 once these incentives were removed, eventually trending below the level of cooperation in the control group. This suggests the possibility of temporary incentives backfiring in the long run. This paper ties in with the literature highlighting the potentially adverse effects of the use of incentives. (C) 2014 Elsevier Inc. All rights reserved. KW - Public good game KW - Team KW - Punishment KW - Incentives KW - Experiment Y1 - 2014 U6 - https://doi.org/10.1016/j.socec.2014.09.001 SN - 2214-8043 SN - 2214-8051 VL - 53 SP - 120 EP - 130 PB - Elsevier CY - New York ER - TY - JOUR A1 - Busch, Jan Philip A1 - Meissner, Tobias A1 - Potthoff, Annegret A1 - Oswald, Sascha T1 - Transport of carbon colloid supported nanoscale zero-valent iron in saturated porous media JF - Journal of contaminant hydrology N2 - Injection of nanoscale zero-valent iron (nZVI) has recently gained great interest as emerging technology for in-situ remediation of chlorinated organic compounds from groundwater systems. Zero-valent iron (ZVI) is able to reduce organic compounds and to render it to less harmful substances. The use of nanoscale particles instead of granular or microscale particles can increase dechlorination rates by-orders of magnitude due to its high surface area. However, classical nZVI appears to be hampered in its environmental application by its limited mobility. One approach is colloid supported transport of nZVI, where the nZVI gets transported by a Mobile colloid. In this study transport properties of activated carbon colloid supported nZVI (c-nZVI; d(50) = 2.4 mu m) are investigated in column tests using columns of 40 cm length, which were filled with porous media. A suspension was pumped through the column under different physicochemical conditions (addition of a polyanionic stabilizer and changes in pH and ionic strength). Highest observed breakthrough was 62% of the injected concentration in glass beads with addition of stabilizer. Addition of mono- and bivalent salt, e.g. more than 0.5 mM/L CaCl2, can decrease mobility and changes in pH to values below six can inhibit mobility at all. Measurements of colloid sizes and zeta potentials show changes in the mean particle size by a factor of ten and an increase of zeta potential from -62 mV to -80 mV during the transport experiment. However, results suggest potential applicability of c-nZVI under field conditions. (C) 2014 Elsevier B.V. All rights reserved. KW - Nanoscale zero-valent iron (nZVI) KW - Nanomaterial KW - Carbo-Iron (R) KW - Colloid transport KW - Mobility KW - In-situ remediation Y1 - 2014 U6 - https://doi.org/10.1016/j.jconhyd.2014.05.006 SN - 0169-7722 SN - 1873-6009 VL - 164 SP - 25 EP - 34 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Busch, Jan Philip A1 - Meissner, Tobias A1 - Potthoff, Annegret A1 - Oswald, Sascha T1 - Investigations on mobility of carbon colloid supported nanoscale zero-valent iron (nZVI) in a column experiment and a laboratory 2D-aquifer test system JF - Environmental science and pollution research : official organ of the EuCheMS Division for Chemistry and the Environment, EuCheMS DCE N2 - Nanoscale zero-valent iron (nZVI) has recently gained great interest in the scientific community as in situ reagent for installation of permeable reactive barriers in aquifer systems, since nZVI is highly reactive with chlorinated compounds and may render them to harmless substances. However, nZVI has a high tendency to agglomerate and sediment; therefore it shows very limited transport ranges. One new approach to overcome the limited transport of nZVI in porous media is using a suited carrier colloid. In this study we tested mobility of a carbon colloid supported nZVI particle "Carbo-Iron Colloids" (CIC) with a mean size of 0.63 mu m in a column experiment of 40 cm length and an experiment in a two-dimensional (2D) aquifer test system with dimensions of 110x40x5 cm. Results show a breakthrough maximum of 82 % of the input concentration in the column experiment and 58 % in the 2D-aquifer test system. Detected residuals in porous media suggest a strong particle deposition in the first centimeters and few depositions in the porous media in the further travel path. Overall, this suggests a high mobility in porous media which might be a significant enhancement compared to bare or polyanionic stabilized nZVI. KW - Carbon colloid KW - Nanoscale zero-valent iron (nZVI) KW - Aquifer systems Y1 - 2014 U6 - https://doi.org/10.1007/s11356-014-3049-7 SN - 0944-1344 SN - 1614-7499 VL - 21 IS - 18 SP - 10908 EP - 10916 PB - Springer CY - Heidelberg ER - TY - JOUR A1 - Böttcher, Steven A1 - Merz, Christoph A1 - Lischeid, Gunnar A1 - Dannowski, Ralf T1 - Using Isomap to differentiate between anthropogenic and natural effects on groundwater dynamics in a complex geological setting JF - Journal of hydrology N2 - Due to increasing demands and competition for high quality groundwater resources in many parts of the world, there is an urgent need for efficient methods that shed light on the interplay between complex natural settings and anthropogenic impacts. Thus a new approach is introduced, that aims to identify and quantify the predominant processes or factors of influence that drive groundwater and lake water dynamics on a catchment scale. The approach involves a non-linear dimension reduction method called Isometric feature mapping (Isomap). This method is applied to time series of groundwater head and lake water level data from a complex geological setting in Northeastern Germany. Two factors explaining more than 95% of the observed spatial variations are identified: (1) the anthropogenic impact of a waterworks in the study area and (2) natural groundwater recharge with different degrees of dampening at the respective sites of observation. The approach enables a presumption-free assessment to be made of the existing geological conception in the catchment, leading to an extension of the conception. Previously unknown hydraulic connections between two aquifers are identified, and connections revealed between surface water bodies and groundwater. (C) 2014 Elsevier B.V. All rights reserved. KW - Groundwater KW - Lake KW - Interaction KW - Isometric feature mapping KW - Time series analysis Y1 - 2014 U6 - https://doi.org/10.1016/j.jhydrol.2014.09.048 SN - 0022-1694 SN - 1879-2707 VL - 519 SP - 1634 EP - 1641 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Bürger, Gerd A1 - Heistermann, Maik A1 - Bronstert, Axel T1 - Towards subdaily rainfall disaggregation via Clausius-Clapeyron JF - Journal of hydrometeorology N2 - Two lines of research are combined in this study: first, the development of tools for the temporal disaggregation of precipitation, and second, some newer results on the exponential scaling of heavy short-term precipitation with temperature, roughly following the Clausius-Clapeyron (CC) relation. Having no extra temperature dependence, the traditional disaggregation schemes are shown to lack the crucial CC-type temperature dependence. The authors introduce a proof-of-concept adjustment of an existing disaggregation tool, the multiplicative cascade model of Olsson, and show that, in principal, it is possible to include temperature dependence in the disaggregation step, resulting in a fairly realistic temperature dependence of the CC type. They conclude by outlining the main calibration steps necessary to develop a full-fledged CC disaggregation scheme and discuss possible applications. Y1 - 2014 U6 - https://doi.org/10.1175/JHM-D-13-0161.1 SN - 1525-755X SN - 1525-7541 VL - 15 IS - 3 SP - 1303 EP - 1311 PB - American Meteorological Soc. CY - Boston ER - TY - THES A1 - Cao, Xianyong T1 - Vegetation and climate change in eastern continental Asia during the last 22 ka inferred from pollen data synthesis Y1 - 2014 ER - TY - JOUR A1 - Cao, Xianyong A1 - Herzschuh, Ulrike A1 - Telford, Richard J. A1 - Ni, Jian T1 - A modern pollen-climate dataset from China and Mongolia: assessing its potential for climate reconstruction JF - Review of palaeobotany and palynology : an international journal N2 - A modern pollen dataset from China and Mongolia (18-52 degrees N, 74-132 degrees E) is investigated for its potential use in climate reconstructions. The dataset includes 2559 samples, 229 terrestrial pollen taxa and four climatic variables - mean annual precipitation (P-ann): 35-2091 mm, mean annual temperature (T-ann): -12.1-25.8 degrees C, mean temperature in the coldest month (Mt(co).): -33.8-21.7 degrees C, and mean temperature in the warmest month (Mt(wa)): 03-29.8 degrees C. Modern pollen-climate relationships are assessed using canonical correspondence analysis (CCA), Huisman-Olff-Fresco (HOF) models, the modern analogue technique (MAT), and weighted averaging partial least squares (WA-PLS). Results indicate that P-ann is the most important climatic determinant of pollen distribution and the most promising climate variable for reconstructions, as assessed by the coefficient of determination between observed and predicted environmental values (r(2)) and root mean square error of prediction (RMSEP). Mt(co) and Mt(wa) may be reconstructed too, but with caution. Samples from different depositional environments influence the performance of cross-validation differently, with samples from lake sediment-surfaces and moss polsters having the best fit with the lowest RMSEP. The better model performances of MAT are most probably caused by spatial autocorrelation. Accordingly, the WA-PLS models of this dataset are deemed most suitable for reconstructing past climate quantitatively because of their more reliable predictive power. (C) 2014 Elsevier B.V. All rights reserved. KW - Calibration KW - Huisman-Olff-Fresco models KW - MAT KW - Pollen-climate transfer function KW - Spatial autocorrelation KW - WA-PLS Y1 - 2014 U6 - https://doi.org/10.1016/j.revpalbo.2014.08.007 SN - 0034-6667 SN - 1879-0615 VL - 211 SP - 87 EP - 96 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Carrapa, Barbara A1 - Mustapha, Fariq Shazanee A1 - Cosca, Michael A1 - Gehrels, George A1 - Schoenbohm, Lindsay M. A1 - Sobel, Edward A1 - DeCelles, Peter G. A1 - Russell, Joellen A1 - Goodman, Paul T1 - Multisystem dating of modern river detritus from Tajikistan and China: Implications for crustal evolution and exhumation of the Pamir JF - Lithosphere N2 - The Pamir is the western continuation of Tibet and the site of some of the highest mountains on Earth, yet comparatively little is known about its crustal and tectonic evolution and erosional history. Both Tibet and the Pamir are characterized by similar terranes and sutures that can be correlated along strike, although the details of such correlations remain controversial. The erosional history of the Pamir with respect to Tibet is significantly different as well: Most of Tibet has been characterized by internal drainage and low erosion rates since the early Cenozoic; in contrast, the Pamir is externally drained and topographically more rugged, and it has a strongly asymmetric drainage pattern. Here, we report 700 new U-Pb and Lu-Hf isotope determinations and >300 Ar-40/Ar-39 ages from detrital minerals derived from rivers in China draining the northeastern Pamir and >1000 apatite fission-track (AFT) ages from 12 rivers in Tajikistan and China draining the northeastern, central, and southern Pamir. U-Pb ages from rivers draining the northeastern Pamir are Mesozoic to Proterozoic and show affinity with the Songpan-Ganzi terrane of northern Tibet, whereas rivers draining the central and southern Pamir are mainly Mesozoic and show some affinity with the Qiangtang terrane of central Tibet. The epsilon(Hf) values are juvenile, between 15 and -5, for the northeastern Pamir and juvenile to moderately evolved, between 10 and -40, for the central and southern Pamir. Detrital mica Ar-40/Ar-39 ages for the northeastern Pamir (eastern drainages) are generally older than ages from the central and southern Pamir (western drainages), indicating younger or lower-magnitude exhumation of the northeastern Pamir compared to the central and southern Pamir. AFT data show strong Miocene-Pliocene signals at the orogen scale, indicating rapid erosion at the regional scale. Despite localized exhumation of the Mustagh-Ata and Kongur-Shan domes, average erosion rates for the northeastern Pamir are up to one order of magnitude lower than erosion rates recorded by the central and southern Pamir. Deeper exhumation of the central and southern Pamir is associated with tectonic exhumation of central Pamir domes. Deeper exhumation coincides with western and asymmetric drainages and with higher precipitation today, suggesting an orographic effect on exhumation. A younging-southward trend of cooling ages may reflect tectonic processes. Overall, cooling ages derived from the Pamir are younger than ages recorded in Tibet, indicating younger and higher magnitudes of erosion in the Pamir. Y1 - 2014 U6 - https://doi.org/10.1130/L360.1 SN - 1941-8264 SN - 1947-4253 VL - 6 IS - 6 SP - 443 EP - 455 PB - Geological Society of America CY - Boulder ER - TY - JOUR A1 - Carrapa, Barbara A1 - Reyes-Bywater, Sharon A1 - Safipour, Roxana A1 - Sobel, Edward A1 - Schoenbohm, Lindsay M. A1 - DeCelles, Peter G. A1 - Reiners, Peter W. A1 - Stockli, Daniel T1 - The effect of inherited paleotopography on exhumation of the Central Andes of NW Argentina JF - Geological Society of America bulletin N2 - Differential exhumation in the Puna Plateau and Eastern Cordillera of NW Argentina is controlled by inherited paleostructures and resulting paleotopography related to the Cretaceous Salta Rift paleomargins. The Ceno zoic deformation front related to the development of the Andean retro-arc orogenic system is generally associated with >4 km of exhumation, which is recorded by Cenozoic apatite fi ssion-track (AFT) and (U-Th-[Sm])/He ages (He ages) in the Eastern Cordillera of NW Argentina. New AFT ages from the top of the Nevado de Cachi document Oligocene (ca. 28 Ma) cooling, which, combined with existing data, indicates exhumation of this range between ca. 28 Ma and ca. 14 Ma. However, some of the highest ranges in the Eastern Cordillera preserve Cretaceous ages indicative of limited Cenozoic exhumation. Samples collected from an similar to 3-km-elevation transect along the northern part of the Sierra de Quilmes paleorift fl ank (Laguna Brava) show AFT ages between ca. 80 and ca. 50 Ma and He ages between ca. 45 and ca. 10 Ma. Another set of samples from an similar to 1-km-elevation transect farther to the southwest (La Quebrada) shows Cretaceous AFT ages between ca. 116 Ma and ca. 76 Ma, and mainly Cretaceous He ages, in agreement with AFT data. Analysis of existing AFT and He ages from the area once occupied by the Salta Rift reveals a pattern characterized by Cretaceous ages along paleorift highs and Cenozoic ages within paleorift hanging-wall basins and later foreland basin depocenters. This pattern is interrupted by the Sierras Pampeanas at similar to 28 degrees S, which record mid-Cenozoic ages. Our data are consistent with a complex inherited pattern of pre-Andean paleostructures, likely associated with paleotopography, which was beveled by the Cenozoic regional foreland basin and reactivated during the late Neogene (ca. <10 Ma), strongly controlling the magnitude of Cenozoic uplift and exhumation and thus cooling age distribution. This, combined with variable lithologic erodibility, resulted in an irregular distribution of themochronological ages. Y1 - 2014 U6 - https://doi.org/10.1130/B30844.1 SN - 0016-7606 SN - 1943-2674 VL - 126 IS - 1-2 SP - 66 EP - 77 PB - American Institute of Physics CY - Boulder ER - TY - JOUR A1 - Cesca, Simone A1 - Grigoli, Francesco A1 - Heimann, Sebastian A1 - Gonzalez, Alvaro A1 - Buforn, Elisa A1 - Maghsoudi, Samira A1 - Blanch, Estefania A1 - Dahm, Torsten T1 - The 2013 September-October seismic sequence offshore Spain: a case of seismicity triggered by gas injection? JF - Geophysical journal international N2 - A spatially localized seismic sequence originated few tens of kilometres offshore the Mediterranean coast of Spain, close to the Ebro river delta, starting on 2013 September 5, and lasting at least until 2013 October. The sequence culminated in a maximal moment magnitude M-w 4.3 earthquake, on 2013 October 1. The most relevant seismogenic feature in the area is the Fosa de Amposta fault system, which includes different strands mapped at different distances to the coast, with a general NE-SW orientation, roughly parallel to the coastline. However, no significant known historical seismicity has involved this fault system in the past. The epicentral region is also located near the offshore platform of the Castor project, where gas is conducted through a pipeline from mainland and where it was recently injected in a depleted oil reservoir, at about 2 km depth. We analyse the temporal evolution of the seismic sequence and use full waveform techniques to derive absolute and relative locations, estimate depths and focal mechanisms for the largest events in the sequence (with magnitude mbLg larger than 3), and compare them to a previous event (2012 April 8, mbLg 3.3) taking place in the same region prior to the gas injection. Moment tensor inversion results show that the overall seismicity in this sequence is characterized by oblique mechanisms with a normal fault component, with a 30A degrees low-dip angle plane oriented NNE-SSW and a subvertical plane oriented NW-SE. The combined analysis of hypocentral location and focal mechanisms could indicate that the seismic sequence corresponds to rupture processes along shallow low-dip surfaces, which could have been triggered by the gas injection in the reservoir, and excludes the activation of the Amposta fault, as its known orientation is inconsistent with focal mechanism results. An alternative scenario includes the iterated triggering of a system of steep faults oriented NW-SE, which were identified by prior marine seismics investigations. KW - Earthquake dynamics KW - Earthquake source observations Y1 - 2014 U6 - https://doi.org/10.1093/gji/ggu172 SN - 0956-540X SN - 1365-246X VL - 198 IS - 2 SP - 941 EP - 953 PB - Oxford Univ. Press CY - Oxford ER - TY - JOUR A1 - Cesca, Simone A1 - Sen, Ali Tolga A1 - Dahm, Torsten T1 - Seismicity monitoring by cluster analysis of moment tensors JF - Geophysical journal international N2 - We suggest a new clustering approach to classify focal mechanisms from large moment tensor catalogues, with the purpose of automatically identify families of earthquakes with similar source geometry, recognize the orientation of most active faults, and detect temporal variations of the rupture processes. The approach differs in comparison to waveform similarity methods since clusters are detected even if they occur in large spatial distances. This approach is particularly helpful to analyse large moment tensor catalogues, as in microseismicity applications, where a manual analysis and classification is not feasible. A flexible algorithm is here proposed: it can handle different metrics, norms, and focal mechanism representations. In particular, the method can handle full moment tensor or constrained source model catalogues, for which different metrics are suggested. The method can account for variable uncertainties of different moment tensor components. We verify the method with synthetic catalogues. An application to real data from mining induced seismicity illustrates possible applications of the method and demonstrate the cluster detection and event classification performance with different moment tensor catalogues. Results proof that main earthquake source types occur on spatially separated faults, and that temporal changes in the number and characterization of focal mechanism clusters are detected. We suggest that moment tensor clustering can help assessing time dependent hazard in mines. KW - Persistence KW - memory KW - correlations KW - clustering KW - Earthquake source observations Y1 - 2014 U6 - https://doi.org/10.1093/gji/ggt492 SN - 0956-540X SN - 1365-246X VL - 196 IS - 3 SP - 1813 EP - 1826 PB - Oxford Univ. Press CY - Oxford ER - TY - JOUR A1 - Craddock, William H. A1 - Kirby, Eric A1 - Zhang, Huiping A1 - Clark, Marin K. A1 - Champagnac, Jean-Daniel A1 - Yuan, Daoyang T1 - Rates and style of Cenozoic deformation around the Gonghe Basin, northeastern Tibetan Plateau JF - Geosphere N2 - The northeastern Tibetan Plateau constitutes a transitional region between the low-relief physiographic plateau to the south and the high-relief ranges of the Qilian Shan to the north. Cenozoic deformation across this margin of the plateau is associated with localized growth of fault-cored mountain ranges and associated basins. Herein, we combine detailed structural analysis of the geometry of range-bounding faults and deformation of foreland basin strata with geomorphic and exhumational records of erosion in hangingwall ranges in order to investigate the magnitude, timing, and style of deformation along the two primary fault systems, the Qinghai Nan Shan and the Gonghe Nan Shan. Structural mapping shows that both ranges have developed above imbricate fans of listric thrust faults, which sole into decollements in the middle crust. Restoration of shortening along balanced cross sections suggests a minimum of 0.8-2.2 km and 5.1-6.9 km of shortening, respectively. Growth strata in the associated foreland basin record the onset of deformation on the two fault systems at ca. 6-10 Ma and ca. 7-10 Ma, respectively, and thus our analysis suggests late Cenozoic shortening rates of 0.2 +0.2/-0.1 km/m.y. and 0.7 +0.3/-0.2 km/m.y. along the north and south sides of Gonghe Basin. Along the Qinghai Nan Shan, these rates are similar to late Pleistocene slip rates of similar to 0.10 +/- 0.04 mm/yr, derived from restoration and dating of a deformed alluvial-fan surface. Collectively, our results imply that deformation along both flanks of the doubly vergent Qilian Shan-Nan Shan initiated by ca. 10 Ma and that subsequent shortening has been relatively steady since that time. Y1 - 2014 U6 - https://doi.org/10.1130/GES01024.1 SN - 1553-040X VL - 10 IS - 6 SP - 1255 EP - 1282 PB - Geological Society of America CY - Boulder ER - TY - JOUR A1 - Crausbay, Shelley A1 - Genderjahn, Steffi A1 - Hotchkiss, Sara A1 - Sachse, Dirk A1 - Kahmen, Ansgar A1 - Arndt, Stefan K. T1 - Vegetation dynamics at the upper reaches of a tropical montane forest are driven by disturbance over the past 7300 years JF - Arctic, antarctic, and alpine research : an interdisciplinary journal N2 - We assessed tropical montane cloud forest (TMCF) sensitivity to natural disturbance by drought, fire, and dieback with a 7300-year-long paleorecord. We analyzed pollen assemblages, charcoal accumulation rates, and higher plant biomarker compounds (average chain length [ACL] of n-alkanes) in sediments from Wai 'anapanapa, a small lake near the upper forest limit and the mean trade wind inversion ('IWI) in Hawai`i. The paleorecord of ACL suggests increased drought frequency and a lower awl elevation from 2555-1323 cal yr B.P. and 606-334 cal yr B.P. Charcoal began to accumulate and a novel fire regime was initiated ca. 880 cal yr B.P., followed by a decreased fire return interval at ca. 550 cal yr B.P. Diebacks occurred at 2931, 2161, 1162, and 306 cal yr B.P., and two of these were independent of drought or fire. Pollen assemblages indicate that on average species composition changed only 2.8% per decade. These dynamics, though slight, were significantly associated with disturbance. The direction of species composition change varied with disturbance type. Drought was associated with significantly more vines and lianas; fire was associated with an increase in the tree fern Sadleria and indicators of open, disturbed landscapes at the expense of epiphytic ferns; whereas stand-scale dieback was associated with an increase in the tree fern Cibotium. Though this cloud forest was dynamic in response to past disturbance, it has recovered, suggesting a resilient TMCF with no evidence of state change in vegetation type (e.g., grassland or shrubland). Y1 - 2014 U6 - https://doi.org/10.1657/1938-4246-46.4.787 SN - 1523-0430 SN - 1938-4246 VL - 46 IS - 4 SP - 787 EP - 799 PB - Institute of Arctic and Alpine Research, University of Colorado CY - Boulder ER - TY - JOUR A1 - Creutzfeldt, Benjamin A1 - Troch, Peter A. A1 - Guentner, Andreas A1 - Ferre, Ty P. A. A1 - Gräff, Thomas A1 - Merz, Bruno T1 - Storage-discharge relationships at different catchment scales based on local high-precision gravimetry JF - Hydrological processes N2 - In hydrology, the storage-discharge relationship is a fundamental catchment property. Understanding what controls this relationship is at the core of catchment science. To date, there are no direct methods to measure water storage at catchment scales (10(1)-10(3)km(2)). In this study, we use direct measurements of terrestrial water storage dynamics by means of superconducting gravimetry in a small headwater catchment of the Regen River, Germany, to derive empirical storage-discharge relationships in nested catchments of increasing scale. Our results show that the local storage measurements are strongly related to streamflow dynamics at larger scales (> 100km(2); correlation coefficient=0.78-0.81), but at small scale, no such relationship exists (similar to 1km(2); correlation coefficients=-0.11). The geologic setting in the region can explain both the disconnection between local water storage and headwater runoff, and the connectivity between headwater storage and streams draining larger catchment areas. More research is required to understand what controls the form of the observed storage-discharge relationships at the catchment scale. This study demonstrates that high-precision gravimetry can provide new insights into the complex relationship between state and response of hydrological systems. KW - water storage KW - high-precision gravimeter KW - storage-discharge relationship KW - nested catchments Y1 - 2014 U6 - https://doi.org/10.1002/hyp.9689 SN - 0885-6087 SN - 1099-1085 VL - 28 IS - 3 SP - 1465 EP - 1475 PB - Wiley-Blackwell CY - Hoboken ER - TY - JOUR A1 - Dahm, Torsten A1 - Fischer, Tomas T1 - Velocity ratio variations in the source region of earthquake swarms in NW Bohemia obtained from arrival time double-differences JF - Geophysical journal international N2 - Crustal earthquake swarms are an expression of intensive cracking and rock damaging over periods of days, weeks or month in a small source region in the crust. They are caused by longer lasting stress changes in the source region. Often, the localized stressing of the crust is associated with fluid or gas migration, possibly in combination with pre-existing zones of weaknesses. However, verifying and quantifying localized fluid movement at depth remains difficult since the area affected is small and geophysical prospecting methods often cannot reach the required resolution. We apply a simple and robust method to estimate the velocity ratio between compressional (P) and shear (S) waves (upsilon(P)/upsilon(S)-ratio) in the source region of an earthquake swarm. The upsilon(P)/upsilon(S)-ratio may be unusual small if the swarm is related to gas in a porous or fractured rock. The method uses arrival time difference between P and S waves observed at surface seismic stations, and the associated double differences between pairs of earthquakes. An advantage is that earthquake locations are not required and the method seems lesser dependent on unknown velocity variations in the crust outside the source region. It is, thus, suited for monitoring purposes. Applications comprise three natural, mid-crustal (8-10 km) earthquake swarms between 1997 and 2008 from the NW-Bohemia swarm region. We resolve a strong temporal decrease of upsilon(P)/upsilon(S) before and during the main activity of the swarm, and a recovery of upsilon(P)/upsilon(S) to background levels at the end of the swarms. The anomalies are interpreted in terms of the Biot-Gassman equations, assuming the presence of oversaturated fluids degassing during the beginning phase of the swarm activity. KW - Tomography KW - Earthquake source observations KW - Volcano seismology Y1 - 2014 U6 - https://doi.org/10.1093/gji/ggt410 SN - 0956-540X SN - 1365-246X VL - 196 IS - 2 SP - 957 EP - 970 PB - Oxford Univ. Press CY - Oxford ER - TY - INPR A1 - de Araujo, Jose Carlos A1 - Batalla Villanueva, Ramon J. A1 - Bronstert, Axel T1 - Special issue: analysis and modelling of sediment transfer in Mediterranean river basins T2 - Journal of soils and sediments : protection, risk assessment and remediation Y1 - 2014 U6 - https://doi.org/10.1007/s11368-014-1000-7 SN - 1439-0108 SN - 1614-7480 VL - 14 IS - 12 SP - 1905 EP - 1908 PB - Springer CY - Heidelberg ER - TY - JOUR A1 - Delgado, Jose Miguel Martins A1 - Merz, Bruno A1 - Apel, Heiko T1 - Projecting flood hazard under climate change: an alternative approach to model chains JF - Natural hazards and earth system sciences N2 - Flood hazard projections under climate change are typically derived by applying model chains consisting of the following elements: "emission scenario - global climate model - downscaling, possibly including bias correction hydrological model - flood frequency analysis". To date, this approach yields very uncertain results, due to the difficulties of global and regional climate models to represent precipitation. The implementation of such model chains requires major efforts, and their complexity is high. We propose for the Mekong River an alternative approach which is based on a shortened model chain: "emission scenario - global climate model - non-stationary flood frequency model". The underlying idea is to use a link between the Western Pacific monsoon and local flood characteristics: the variance of the monsoon drives a non-stationary flood frequency model, yielding a direct estimate of flood probabilities. This approach bypasses the uncertain precipitation, since the monsoon variance is derived from large-scale wind fields which are better represented by climate models. The simplicity of the monsoon-flood link allows deriving large ensembles of flood projections under climate change. We conclude that this is a worthwhile, complementary approach to the typical model chains in catchments where a substantial link between climate and floods is found. Y1 - 2014 U6 - https://doi.org/10.5194/nhess-14-1579-2014 SN - 1561-8633 VL - 14 IS - 6 SP - 1579 EP - 1589 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Deplazes, Gaudenz A1 - Lückge, Andreas A1 - Stuut, Jan-Berend W. A1 - Paetzold, Jürgen A1 - Kuhlmann, Holger A1 - Husson, Dorothee A1 - Fant, Mara A1 - Haug, Gerald H. T1 - Weakening and strengthening of the Indian monsoon during Heinrich events and Dansgaard- Oeschger oscillations JF - Paleoceanography N2 - The Dansgaard-Oeschger oscillations and Heinrich events described in North Atlantic sediments and Greenland ice are expressed in the climate of the tropics, for example, as documented in Arabian Sea sediments. Given the strength of this teleconnection, we seek to reconstruct its range of environmental impacts. We present geochemical and sedimentological data from core SO130-289KL from the Indus submarine slope spanning the last similar to 80 kyr. Elemental and grain size analyses consistently indicate that interstadials are characterized by an increased contribution of fluvial suspension from the Indus River. In contrast, stadials are characterized by an increased contribution of aeolian dust from the Arabian Peninsula. Decadal-scale shifts at climate transitions, such as onsets of interstadials, were coeval with changes in productivity-related proxies. Heinrich events stand out as especially dry and dusty events, indicating a dramatically weakened Indian summer monsoon, potentially increased winter monsoon circulation, and increased aridity on the Arabian Peninsula. This finding is consistent with other paleoclimate evidence for continental aridity in the northern tropics during these events. Our results strengthen the evidence that circum-North Atlantic temperature variations translate to hydrological shifts in the tropics, with major impacts on regional environmental conditions such as rainfall, river discharge, aeolian dust transport, and ocean margin anoxia. KW - Indian Monsoon KW - Arabian Sea KW - XRF KW - Dansgaard-Oeschger oscillations KW - Heinrich events KW - Sediment Transport Y1 - 2014 U6 - https://doi.org/10.1002/2013PA002509 SN - 0883-8305 SN - 1944-9186 VL - 29 IS - 2 SP - 99 EP - 114 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Dietze, Elisabeth A1 - Maussion, F. A1 - Ahlborn, M. A1 - Diekmann, Bernhard A1 - Hartmann, K. A1 - Henkel, K. A1 - Kasper, T. A1 - Lockot, G. A1 - Opitz, S. A1 - Haberzettl, T. T1 - Sediment transport processes across the Tibetan Plateau inferred from robust grain-size end members in lake sediments JF - Climate of the past : an interactive open access journal of the European Geosciences Union N2 - Grain-size distributions offer powerful proxies of past environmental conditions that are related to sediment sorting processes. However, they are often of multimodal character because sediments can get mixed during deposition. To facilitate the use of grain size as palaeoenvironmental proxy, this study aims to distinguish the main detrital processes that contribute to lacustrine sedimentation across the Tibetan Plateau using grain-size end-member modelling analysis. Between three and five robust grain-size end-member subpopulations were distinguished at different sites from similarly-likely end-member model runs. Their main modes were grouped and linked to common sediment transport and depositional processes that can be associated with contemporary Tibetan climate (precipitation patterns and lake ice phenology, gridded wind and shear stress data from the High Asia Reanalysis) and local catchment configurations. The coarse sands and clays with grain-size modes > 250 mu m and < 2 mu m were probably transported by fluvial processes. Aeolian sands (similar to 200 mu m) and coarse local dust (similar to 60 mu m), transported by saltation and in near-surface suspension clouds, are probably related to occasional westerly storms in winter and spring. Coarse regional dust with modes similar to 25 mu m may derive from near-by sources that keep in longer term suspension. The continuous background dust is differentiated into two robust end members (modes: 5-10 and 2-5 mu m) that may represent different sources, wind directions and/or sediment trapping dynamics from long-range, upper-level westerly and episodic northerly wind transport. According to this study grain-size end members of only fluvial origin contribute small amounts to mean Tibetan lake sedimentation (19 +/- 5%), whereas local to regional aeolian transport and background dust deposition dominate the clastic sedimentation in Tibetan lakes (contributions: 42 +/- 14% and 51 +/- 11%). However, fluvial and alluvial reworking of aeolian material from nearby slopes during summer seems to limit end-member interpretation and should be cross-checked with other proxy information. If not considered as a stand-alone proxy, a high transferability to other regions and sediment archives allows helpful reconstructions of past sedimentation history. Y1 - 2014 U6 - https://doi.org/10.5194/cp-10-91-2014 SN - 1814-9324 SN - 1814-9332 VL - 10 IS - 1 SP - 91 EP - 106 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Donner, Stefanie A1 - Krüger, Frank A1 - Roessler, Dirk A1 - Ghods, Abdolreza T1 - Combined Inversion of broadband and short-period waveform data for regional moment tensors: A case study in the Alborz Mountains, Iran JF - Bulletin of the Seismological Society of America N2 - In this study, we suggest a novel approach for the retrieval of regional moment tensors for earthquakes with small to moderate magnitudes. The first modification is the combined inversion of broadband and short-period waveform data. The broadband waveforms are inverted in a frequency range suitable for surface waves, whereas for the short-period data a frequency range suitable for body waves is applied. The second modification is the use of first-motion body-wave polarities to select the most probable solution out of all solutions from inversion. To combine three different criteria for selecting the most probable solution (i.e., residual from inversion, double-couple content of solution, number of nonmatching first-motion body-wave polarities), the L2 norm is applied to the normalized parameters. We chose five earthquakes within the Alborz mountains, Iran, as a case study (3.1 <= M-w <= 4.1). In this area, several factors exacerbate the difficulty of performing inversion for moment tensors, for example, a heterogeneous station network and large azimuthal gaps. We have demonstrated that our approach supplies reliable moment tensors when inversion from broadband data alone fails. In one case, we successfully retrieved a stable solution from short-period waveform data alone. Thus, our approach enables successful determination of seismic moment tensors wherever a sparse network of broadband stations has thus far prevented it. Y1 - 2014 U6 - https://doi.org/10.1785/0120130229 SN - 0037-1106 SN - 1943-3573 VL - 104 IS - 3 SP - 1358 EP - 1373 PB - Seismological Society of America CY - Albany ER - TY - JOUR A1 - Douglas, John A1 - Akkar, Sinan A1 - Ameri, Gabriele A1 - Bard, Pierre-Yves A1 - Bindi, Dino A1 - Bommer, Julian J. A1 - Bora, Sanjay Singh A1 - Cotton, Fabrice Pierre A1 - Derras, Boumediene A1 - Hermkes, Marcel A1 - Kuehn, Nicolas Martin A1 - Luzi, Lucia A1 - Massa, Marco A1 - Pacor, Francesca A1 - Riggelsen, Carsten A1 - Sandikkaya, M. Abdullah A1 - Scherbaum, Frank A1 - Stafford, Peter J. A1 - Traversa, Paola T1 - Comparisons among the five ground-motion models developed using RESORCE for the prediction of response spectral accelerations due to earthquakes in Europe and the Middle East JF - Bulletin of earthquake engineering : official publication of the European Association for Earthquake Engineering N2 - This article presents comparisons among the five ground-motion models described in other articles within this special issue, in terms of data selection criteria, characteristics of the models and predicted peak ground and response spectral accelerations. Comparisons are also made with predictions from the Next Generation Attenuation (NGA) models to which the models presented here have similarities (e.g. a common master database has been used) but also differences (e.g. some models in this issue are nonparametric). As a result of the differing data selection criteria and derivation techniques the predicted median ground motions show considerable differences (up to a factor of two for certain scenarios), particularly for magnitudes and distances close to or beyond the range of the available observations. The predicted influence of style-of-faulting shows much variation among models whereas site amplification factors are more similar, with peak amplification at around 1s. These differences are greater than those among predictions from the NGA models. The models for aleatory variability (sigma), however, are similar and suggest that ground-motion variability from this region is slightly higher than that predicted by the NGA models, based primarily on data from California and Taiwan. KW - Strong-motion data KW - Ground-motion models KW - Ground-motion prediction equations KW - Style of faulting KW - Site amplification KW - Aleatory variability KW - Epistemic uncertainty KW - Europe KW - Middle East Y1 - 2014 U6 - https://doi.org/10.1007/s10518-013-9522-8 SN - 1570-761X SN - 1573-1456 VL - 12 IS - 1 SP - 341 EP - 358 PB - Springer CY - Dordrecht ER - TY - JOUR A1 - Duesterhoeft, Erik A1 - Quinteros, Javier A1 - Oberhänsli, Roland A1 - Bousquet, Romain A1 - de Capitani, Christian T1 - Relative impact of mantle densification and eclogitization of slabs on subduction dynamics: A numerical thermodynamic/thermokinematic investigation of metamorphic density evolution JF - Tectonophysics : international journal of geotectonics and the geology and physics of the interior of the earth N2 - Understanding the relationships between density and spatio-thermal variations at convergent plate boundaries is important for deciphering the present-day dynamics and evolution of subduction zones. In particular, the interaction between densification due to mineralogical phase transitions and slab pull forces is subject to ongoing investigations. We have developed a two-dimensional subduction zone model that is based on thermodynamic equilibrium assemblage calculations and includes the effects of melting processes on the density distribution in the lithosphere. Our model calculates the "metamorphic density" of rocks as a function of pressure, temperature and chemical composition in a subduction zone down to 250 km. We have used this model to show how the hydration, dehydration, partial melting and fractionation processes of rocks all influence the metamorphic density and greatly depend on the temperature field within the subduction system. These processes are largely neglected by other approaches that reproduce the density distribution within this complex tectonic setting. Our model demonstrates that the initiation of edogitization (i.e., when crustal rocks reach higher densities than the ambient mantle) of the slab is not the only significant process that makes the descending slab denser and generates the slab pull force. Instead, the densification of the lithospheric mantle of the sinking slab starts earlier than eclogitization and contributes significantly to slab pull in the early stages of subduction. Accordingly, the complex metamorphic structure of the slab and the mantle wedge has an important impact on the development of subduction zones. (C) 2014 Elsevier B.V. All rights reserved. KW - Density KW - Melt KW - Metamorphism KW - Subduction KW - Thermodynamic modeling KW - Thermo-mechanical modeling Y1 - 2014 U6 - https://doi.org/10.1016/j.tecto.2014.09.009 SN - 0040-1951 SN - 1879-3266 VL - 637 SP - 20 EP - 29 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Dulanya, Zuze A1 - Croudace, Ian A1 - Reed, Jane M. A1 - Trauth, Martin H. T1 - Palaeolimnological reconstruction of recent environmental change in Lake Malombe (S. Malawi) using multiple proxies JF - Water SA N2 - Shallow inland water bodies in Malawi continue to be threatened by various environmental challenges despite their importance to the fisheries industry. Due to the complex interaction between natural and anthropogenic disturbances, disentangling the effect of the two may be a complicated process. The littoral zone of most water bodies is important in environmental reconstructions including pollution and lake level monitoring. This study used a littoral zone, transect-based approach employing multi-proxy palaeolimnological techniques to reconstruct recent environmental change (ca. 100 yrs.) in Lake Malombe in the Malawi Rift, East Africa. The results of the study could inform fisheries management in Lake Malombe, which experienced a catastrophic decline in fish stocks. Results support documentary evidence for the complete desiccation of the lake less than 100 years ago. Subsequently, there is evidence for accelerated eutrophication in the recent past. In light of these results, it is concluded that transect sampling approaches rather than relying on single core measurements, and the need for careful consideration of the types of proxy, are significant considerations in palaeoenvironmental reconstructions. KW - littoral zone KW - palaeolimnology KW - diatoms KW - Lake Malombe Y1 - 2014 U6 - https://doi.org/10.4314/wsa.v40i4.17 SN - 0378-4738 SN - 1816-7950 VL - 40 IS - 4 SP - 717 EP - 727 PB - Water Research Commission CY - Pretoria ER - TY - JOUR A1 - Eroglu, Deniz A1 - Marwan, Norbert A1 - Prasad, Sushma A1 - Kurths, Jürgen T1 - Finding recurrence networks' threshold adaptively for a specific time series JF - Nonlinear processes in geophysics N2 - Recurrence-plot-based recurrence networks are an approach used to analyze time series using a complex networks theory. In both approaches - recurrence plots and recurrence networks -, a threshold to identify recurrent states is required. The selection of the threshold is important in order to avoid bias of the recurrence network results. In this paper, we propose a novel method to choose a recurrence threshold adaptively. We show a comparison between the constant threshold and adaptive threshold cases to study period-chaos and even period-period transitions in the dynamics of a prototypical model system. This novel method is then used to identify climate transitions from a lake sediment record. Y1 - 2014 U6 - https://doi.org/10.5194/npg-21-1085-2014 SN - 1023-5809 VL - 21 IS - 6 SP - 1085 EP - 1092 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Fahle, Marcus A1 - Dietrich, Ottfried T1 - Estimation of evapotranspiration using diurnal groundwater level fluctuations: Comparison of different approaches with groundwater lysimeter data JF - Water resources research N2 - In wetlands or riparian areas, water withdrawal by plants with access to groundwater or the capillary fringe often causes diurnal groundwater fluctuations. Various approaches use the characteristics of these fluctuations for estimation of daily groundwater evapotranspiration rates. The objective of this paper was to review the available methods, compare them with measured evapotranspiration and assess their recharge assumptions. For this purpose, we employed data of 85 rain-free days of a weighable groundwater lysimeter situated at a grassland site in the Spreewald wetland in north-east Germany. Measurements of hourly recharge and daily evapotranspiration rates were used to assess the different approaches. Our results showed that a maximum of 50% of the day to day variance of the daily evapotranspiration rates could be explained by the approaches based on groundwater fluctuations. Simple and more complex methods performed similarly. For some of the approaches, there were indications that erroneous assumptions compensated each other (e.g., when overestimated recharge counteracted underestimated storage change). We found that the usage of longer time spans resulted in improved estimates of the daily recharge rates and that the estimates were further enhanced by including two night averages. When derived from fitting estimates of recharge or evapotranspiration with according measurements the specific yield, needed to convert changes in water level to water volumes, differed considerably among the methods (from 0.022 to 0.064). Thus, the specific yield can be seen as correction factor that compensates for inadequate process descriptions. KW - evapotranspiration KW - groundwater lysimeter KW - specific yield KW - diurnal signal KW - phreatophytes KW - wetland Y1 - 2014 U6 - https://doi.org/10.1002/2013WR014472 SN - 0043-1397 SN - 1944-7973 VL - 50 IS - 1 SP - 273 EP - 286 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Farinotti, Daniel A1 - King, Edward C. A1 - Albrecht, Anika A1 - Huss, Matthias A1 - Gudmundsson, Gudmundur Hilmar T1 - The bedrock topography of Starbuck Glacier, Antarctic Peninsula, as determined by radio-echo soundings and flow modeling JF - Annals of glaciology KW - Antarctic glaciology KW - glaciological instruments and methods KW - ground-penetrating radar KW - ice-shelf tributary glaciers KW - radio-echo sounding Y1 - 2014 U6 - https://doi.org/10.3189/2014AoG67A025 SN - 0260-3055 SN - 1727-5644 VL - 55 IS - 67 SP - 22 EP - 28 PB - International Glaciological Society CY - Cambridge ER - TY - THES A1 - Feld, Christian T1 - Crustal structure of the Eratosthenes Seamount, Cyprus and S. Turkey from an amphibian wide-angle seismic profile T1 - Die Krustenstruktur von dem Eratosthenes Seeberg, Zypern und der Süd-Türkei anhand eines amphibischen seismischen Weitwinkel Profils N2 - In March 2010, the project CoCoCo (incipient COntinent-COntinent COllision) recorded a 650 km long amphibian N-S wide-angle seismic profile, extending from the Eratosthenes Seamount (ESM) across Cyprus and southern Turkey to the Anatolian plateau. The aim of the project is to reveal the impact of the transition from subduction to continent-continent collision of the African plate with the Cyprus-Anatolian plate. A visual quality check, frequency analysis and filtering were applied to the seismic data and reveal a good data quality. Subsequent first break picking, finite-differences ray tracing and inversion of the offshore wide-angle data leads to a first-arrival tomographic model. This model reveals (1) P-wave velocities lower than 6.5 km/s in the crust, (2) a variable crustal thickness of about 28 - 37 km and (3) an upper crustal reflection at 5 km depth beneath the ESM. Two land shots on Turkey, also recorded on Cyprus, airgun shots south of Cyprus and geological and previous seismic investigations provide the information to derive a layered velocity model beneath the Anatolian plateau and for the ophiolite complex on Cyprus. The analysis of the reflections provides evidence for a north-dipping plate subducting beneath Cyprus. The main features of this layered velocity model are (1) an upper and lower crust with large lateral changes of the velocity structure and thickness, (2) a Moho depth of about 38 - 45 km beneath the Anatolian plateau, (3) a shallow north-dipping subducting plate below Cyprus with an increasing dip and (4) a typical ophiolite sequence on Cyprus with a total thickness of about 12 km. The offshore-onshore seismic data complete and improve the information about the velocity structure beneath Cyprus and the deeper part of the offshore tomographic model. Thus, the wide-angle seismic data provide detailed insights into the 2-D geometry and velocity structures of the uplifted and overriding Cyprus-Anatolian plate. Subsequent gravity modelling confirms and extends the crustal P-wave velocity model. The deeper part of the subducting plate is constrained by the gravity data and has a dip angle of ~ 28°. Finally, an integrated analysis of the geophysical and geological information allows a comprehensive interpretation of the crustal structure related to the collision process. N2 - Im März 2010 wurden im Rahmen des "CoCoCo"-Projektes ein 650km langes amphibisches, seismisches Weitwinkel Profil aufgenommen. Dieses erstreckte sich von dem Eratosthenes Seeberg (ESM) über Zypern und der Süd-Türkei bis zum anatolischen Plateau. Das Hauptziel des Projektes ist es, den Einfluss zu untersuchen, der von dem Übergang eines Subduktion Prozesses hin zu einer Kontinent-Kontinent Kollision der afrikanischen Platte mit der zyprisch-anatolischen Platte hervorgerufen wird. Die seismischen Daten wurden einer visuelle Qualitätsüberprüfung, Frequenz-Analyse und Filterung unterzogen und zeigten eine gute Qualität. Das darauf folgende Picken der Ersteinstätze, eine Finite-Differenzen Raytracing und eine Inversion der offshore Weitwinkel Daten, führte zu einem Laufzeit Tomographie Model. Das Modell zeigt (1) P-Wellengeschwindigkeiten kleiner als 6.5 km/s in der Kruste, (2) eine variable Krustenmächtigkeit von 28 - 37 km und (3) eine obere Krustenreflektion in 5 km Tiefe unter dem ESM. Zwei Landschüsse in der Türkei, ebenfalls aufgenommen auf Zypern, Luftkanonen-Schüsse südlich von Zypern und vorausgegangene geologische und seismische Untersuchungen lieferten die Grundlage, um ein geschichtetes Geschwindigkeitsmodell für das anatolische Plateau und für den Ophiolith-Komplex auf Zypern abzuleiten. Die Analyse der Reflexionen liefert den Beweis für eine nach Norden einfallende Platte welche unter Zypern subduziert. Die Hauptkennzeichen dieses geschichteten Geschwindigkeitsmodelles sind (1) eine obere und untere Kruste mit starken lateral Änderungen in Geschwindigkeit und Mächtigkeit, (2) eine Mohotiefe in 38 - 45 km unter dem anatolischen Plateau, (3) eine flach nach Norden einfallende Platte unter Zypern mit ansteigendem Einfallwinkel und (4) eine typische Ophiolith Sequenz auf Zypern mit einer Gesamtmächtigkeit von 12 km. Die seismischen offshore / onshore Daten komplettieren und verbessern die bisherigen Kenntnisse über die Geschwindigkeitsstruktur unter Zypern und des tieferen Bereiches der offshore Tomographie. Damit liefert die Weitwinkel Seismik detaillierte Einblicke in die 2-D Geometrie und die Geschwindigkeitsstrukturen der angehobenen und überlagerten zyprisch-anatolischen Platte. Die darauf folgende Gravimetrie Modellierung bestätigt und erweitert das P-Wellen Krusten-Geschwindigkeits Modell. Der tiefere Teil der subduzierten Platte, welche einen Einfallswinkel von ~ 28° hat, wurde durch die Gravimetrie Daten belegt. Letztlich erlaubt eine ganzheitliche Analyse von geophysikalischen und geologischen Informationen die umfassende Interpretation der Krustenstruktur welche in Verbindung mit dem Kollisions Prozess steht. KW - incipient continent-continent collision KW - crustal structure of the Eratosthenes Seamount KW - controlled source wide angle seismic KW - crustal structure of south central Turkey KW - Cyprus arc KW - aktive Weitewinkel-Seismik KW - Krustenstruktur des Eratosthenes Seeberges KW - beginnende Kontinent-Kontinent Kollision KW - Krustenstruktur der Süd-Türkei KW - Zypernbogen Y1 - 2014 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-73479 ER - TY - JOUR A1 - Feldmann, J. A1 - Albrecht, Torsten A1 - Khroulev, C. A1 - Pattyn, F. A1 - Levermann, Anders T1 - Resolution-dependent performance of grounding line motion in a shallow model compared with a full-Stokes model according to the MISMIP3d intercomparison JF - Journal of glaciology N2 - Making confident statements about the evolution of an ice-sheet shelf system with a numerical model requires the capability to reproduce the migration of the grounding line. Here we show that the shallow-ice approximation/shallow-shelf approximation hybrid-type Parallel Ice Sheet Model (PISM), with its recent improvements, is capable of modeling the grounding line motion in a perturbed ice-sheet shelf system. The model is set up according to the three-dimensional Marine Ice-Sheet Model Intercomparison Project (MISMIP3d), and simulations are carried out across a broad range of spatial resolutions. Using (1) a linear interpolation of the grounding line with locally interpolated basal friction and (2) an improved driving-stress computation across the grounding line, the reversibility of the grounding line (i.e. its retreat after an advance forced by a local perturbation of basal resistance) is captured by the model even at medium and low resolutions (Delta x > 10 km). The transient model response is qualitatively similar to that of higher-order models but reveals a higher initial sensitivity to perturbations on very short timescales. Our findings support the application of PISM to the Antarctic ice sheet from regional up to continental scales and on relatively low spatial resolutions. KW - glacier flow KW - ice dynamics KW - ice-sheet modelling Y1 - 2014 U6 - https://doi.org/10.3189/2014JoG13J093 SN - 0022-1430 SN - 1727-5652 VL - 60 IS - 220 SP - 353 EP - 360 PB - International Glaciological Society CY - Cambridge ER - TY - JOUR A1 - Ferrero, Silvio A1 - Braga, R. A1 - Berkesi, M. A1 - Cesare, Bernardo A1 - Ouazaa, N. Laridhi T1 - Production of metaluminous melt during fluid-present anatexis: an example from the Maghrebian basement, La Galite Archipelago, central Mediterranean JF - Journal of metamorphic geology N2 - Garnet brought to the surface by late Miocene granitoids at La Galite Archipelago (Central Mediterranean, Tunisia) contains abundant primary melt and fluid inclusions. Microstructural observations and mineral chemistry define the host garnet as a peritectic phase produced by biotite incongruent melting at ~800 degrees C and 0.5GPa, under fluid-present conditions. The trapped melt is leucogranitic with an unexpected metaluminous and almost peralkaline character. Fluid inclusions are one phase at room temperature, and contain a CO2-dominated fluid, with minor H2O, N-2 and CH4. Siderite and an OH-bearing phase were identified by Raman and IR spectroscopy within every analysed inclusion, and are interpreted as products of a post-entrapment carbonation/hydration reaction between the fluid and the host during cooling. The fluid present during anatexis is therefore inferred to have been originally richer in both H2O and CO2. The production of anatectic melt with a metaluminous signature can be explained as the result of partial melting of relatively Al-poor protoliths assisted by CO2-rich fluids. KW - fluid inclusions KW - garnet KW - anatexis KW - nanogranites KW - melt inclusions Y1 - 2014 U6 - https://doi.org/10.1111/jmg.12068 SN - 0263-4929 SN - 1525-1314 VL - 32 IS - 2 SP - 209 EP - 225 PB - Wiley-Blackwell CY - Hoboken ER - TY - JOUR A1 - Francke, Till A1 - Werb, Sandra A1 - Sommerer, Erik A1 - Lopez-Tarazon, José Andrés T1 - Analysis of runoff, sediment dynamics and sediment yield of subcatchments in the highly erodible Isabena catchment, Central Pyrenees JF - Journal of soils and sediments : protection, risk assessment and remediation N2 - The Isabena catchment (445 km(2)), Spain, features highly diverse spatial heterogeneity in land use, lithology and rainfall. Consequently, the relative contribution in terms of water and sediment yield varies immensely between its subcatchments, and also temporally. This study presents the synthesis of similar to 2.5 years of monitoring rainfall, discharge and suspended sediment concentration (SSC) in the five main subcatchments of the Isabena and its outlet. Continuous discharge at the subcatchment outlets, nine tipping bucket rainfall and automatic SSC samplers (complemented by manual samples), were collected from June 2011 until November 2013. The water stage records were converted to discharge using a rating curve derived with Bayesian regression. For reconstructing sediment yields, the data from the intermittent SSC sampling needed to be interpolated. We employed non-parametric multivariate regression (Quantile Regression Forests, QRF) using the discharge and rainfall data plus different aggregation levels of these as ancillary predictors. The subsequent Monte Carlo simulations allowed the determination of monthly sediment yields and their uncertainty. The Isabena catchment shows high erosion dynamics with great variability in space and time, with stark contrasts even between adjacent subcatchments. The natural conditions make water and sediment monitoring and instrumentation very challenging; the measurement of discharge is particularly prone to considerable uncertainties. The QRF method employed for reconstructing sedigraphs and monthly yields proved well suited for the task. KW - Mediterranean-mountainous KW - Non-parametric regression KW - Sediment yield KW - Water yield KW - Badlands Y1 - 2014 U6 - https://doi.org/10.1007/s11368-014-0990-5 SN - 1439-0108 SN - 1614-7480 VL - 14 IS - 12 SP - 1909 EP - 1920 PB - Springer CY - Heidelberg ER - TY - JOUR A1 - Frank-Fahle, Beatrice A. A1 - Yergeau, Etienne A1 - Greer, Charles W. A1 - Lantuit, Hugues A1 - Wagner, Dirk T1 - Microbial functional potential and community composition in permafrost-affected soils of the NW canadian arctic JF - PLoS one N2 - Permafrost-affected soils are among the most obvious ecosystems in which current microbial controls on organic matter decomposition are changing as a result of global warming. Warmer conditions in polygonal tundra will lead to a deepening of the seasonal active layer, provoking changes in microbial processes and possibly resulting in exacerbated carbon degradation under increasing anoxic conditions. To identify current microbial assemblages in carbon rich, water saturated permafrost environments, four polygonal tundra sites were investigated on Herschel Island and the Yukon Coast, Western Canadian Arctic. Ion Torrent sequencing of bacterial and archaeal 16S rRNA amplicons revealed the presence of all major microbial soil groups and indicated a local, vertical heterogeneity of the polygonal tundra soil community with increasing depth. Microbial diversity was found to be highest in the surface layers, decreasing towards the permafrost table. Quantitative PCR analysis of functional genes involved in carbon and nitrogen-cycling revealed a high functional potential in the surface layers, decreasing with increasing active layer depth. We observed that soil properties driving microbial diversity and functional potential varied in each study site. These results highlight the small-scale heterogeneity of geomorphologically comparable sites, greatly restricting generalizations about the fate of permafrost-affected environments in a warming Arctic. Y1 - 2014 U6 - https://doi.org/10.1371/journal.pone.0084761 SN - 1932-6203 VL - 9 IS - 1 PB - PLoS CY - San Fransisco ER - TY - JOUR A1 - Freundt, A. A1 - Grevemeyer, I. A1 - Rabbel, W. A1 - Hansteen, T. H. A1 - Hensen, C. A1 - Wehrmann, H. A1 - Kutterolf, S. A1 - Halama, Ralf A1 - Frische, M. T1 - Volatile (H2O, CO2, Cl, S) budget of the Central American subduction zone JF - International journal of earth sciences N2 - After more than a decade of multidisciplinary studies of the Central American subduction zone mainly in the framework of two large research programmes, the US MARGINS program and the German Collaborative Research Center SFB 574, we here review and interpret the data pertinent to quantify the cycling of mineral-bound volatiles (H2O, CO2, Cl, S) through this subduction system. For input-flux calculations, we divide the Middle America Trench into four segments differing in convergence rate and slab lithological profiles, use the latest evidence for mantle serpentinization of the Cocos slab approaching the trench, and for the first time explicitly include subduction erosion of forearc basement. Resulting input fluxes are 40-62 (53) Tg/Ma/m H2O, 7.8-11.4 (9.3) Tg/Ma/m CO2, 1.3-1.9 (1.6) Tg/Ma/m Cl, and 1.3-2.1 (1.6) Tg/Ma/m S (bracketed are mean values for entire trench length). Output by cold seeps on the forearc amounts to 0.625-1.25 Tg/Ma/m H2O partly derived from the slab sediments as determined by geochemical analyses of fluids and carbonates. The major volatile output occurs at the Central American volcanic arc that is divided into ten arc segments by dextral strike-slip tectonics. Based on volcanic edifice and widespread tephra volumes as well as calculated parental magma masses needed to form observed evolved compositions, we determine long-term (10(5) years) average magma and K2O fluxes for each of the ten segments as 32-242 (106) Tg/Ma/m magma and 0.28-2.91 (1.38) Tg/Ma/m K2O (bracketed are mean values for entire Central American volcanic arc length). Volatile/K2O concentration ratios derived from melt inclusion analyses and petrologic modelling then allow to calculate volatile fluxes as 1.02-14.3 (6.2) Tg/Ma/m H2O, 0.02-0.45 (0.17) Tg/Ma/m CO2, and 0.07-0.34 (0.22) Tg/Ma/m Cl. The same approach yields long-term sulfur fluxes of 0.12-1.08 (0.54) Tg/Ma/m while present-day open-vent SO2-flux monitoring yields 0.06-2.37 (0.83) Tg/Ma/m S. Input-output comparisons show that the arc water fluxes only account for up to 40 % of the input even if we include an "invisible" plutonic component constrained by crustal growth. With 20-30 % of the H2O input transferred into the deeper mantle as suggested by petrologic modeling, there remains a deficiency of, say, 30-40 % in the water budget. At least some of this water is transferred into two upper-plate regions of low seismic velocity and electrical resistivity whose sizes vary along arc: one region widely envelopes the melt ascent paths from slab top to arc and the other extends obliquely from the slab below the forearc to below the arc. Whether these reservoirs are transient or steady remains unknown. KW - Subduction input KW - Forearc dewatering KW - Arc magmatism KW - Subduction fluids Y1 - 2014 U6 - https://doi.org/10.1007/s00531-014-1001-1 SN - 1437-3254 SN - 1437-3262 VL - 103 IS - 7 SP - 2101 EP - 2127 PB - Springer CY - New York ER -