TY  - GEN
A1  - Rohrmann, Alexander
A1  - Heermance, Richard
A1  - Kapp, Paul
A1  - Cai, Fulong
T1  - Wind as the primary driver of erosion in the Qaidam Basin, China (vol 374, pg 1, 2013)
T2  - Earth & planetary science letters
Y1  - 2015
U6  - https://doi.org/10.1016/j.epsl.2015.10.011
SN  - 0012-821X
SN  - 1385-013X
VL  - 432
SP  - 501
EP  - 501
PB  - Elsevier
CY  - Amsterdam
ER  - 
TY  - GEN
A1  - Reimold, W. U.
A1  - Schulz, Toni
A1  - Hoffmann, M.
A1  - Wannek, Dshamilja
A1  - Hauser, N.
A1  - van Acken, David
A1  - Luguet, A.
T1  - VREDEFORT GRANOPHYRE GENESIS: CLUES FROM RE-OS ISOTOPE DATA
T2  - Physical review : E, Statistical, nonlinear and soft matter physics
Y1  - 2016
SN  - 1086-9379
SN  - 1945-5100
VL  - 51
SP  - A533
EP  - A533
PB  - Wiley-Blackwell
CY  - Hoboken
ER  - 
TY  - GEN
A1  - Kneis, David
A1  - Abon, Catherine Cristobal
A1  - Bronstert, Axel
A1  - Heistermann, Maik
T1  - Verification of short-term runoff forecasts for a small Philippine basin (Marikina)
T2  - Hydrological sciences journal = Journal des sciences hydrologiques
N2  - Storm runoff from the Marikina River Basin frequently causes flood events in the Philippine capital region Metro Manila. This paper presents and evaluates a system to predict short-term runoff from the upper part of that basin (380km(2)). It was designed as a possible component of an operational warning system yet to be installed. For the purpose of forecast verification, hindcasts of streamflow were generated for a period of 15 months with a time-continuous, conceptual hydrological model. The latter was fed with real-time observations of rainfall. Both ground observations and weather radar data were tested as rainfall forcings. The radar-based precipitation estimates clearly outperformed the raingauge-based estimates in the hydrological verification. Nevertheless, the quality of the deterministic short-term runoff forecasts was found to be limited. For the radar-based predictions, the reduction of variance for lead times of 1, 2 and 3hours was 0.61, 0.62 and 0.54, respectively, with reference to a no-forecast scenario, i.e. persistence. The probability of detection for major increases in streamflow was typically less than 0.5. Given the significance of flood events in the Marikina Basin, more effort needs to be put into the reduction of forecast errors and the quantification of remaining uncertainties.
Y1  - 2016
U6  - https://doi.org/10.1080/02626667.2016.1183773
SN  - 0262-6667
SN  - 2150-3435
VL  - 62
SP  - 205
EP  - 216
PB  - Oxford Univ. Press
CY  - Oxford
ER  - 
TY  - GEN
A1  - Smith, Taylor
A1  - Bookhagen, Bodo
T1  - Using passive microwave data to understand spatio-temporal trends and dynamics in snow-water storage in High Mountain Asia
T2  - active and passive microwave remote sensing for environmental monitoring II
N2  - High Mountain Asia provides water for more than a billion downstream users. Many catchments receive the majority of their yearly water budget in the form of snow - the vast majority of which is not monitored by sparse weather networks. We leverage passive microwave data from the SSMI series of satellites (SSMI, SSMI/S, 1987-2016), reprocessed to 3.125 km resolution, to examine trends in the volume and spatial distribution of snow-water equivalent (SWE) in the Indus Basin. We find that the majority of the Indus has seen an increase in snow-water storage. There exists a strong elevation-trend relationship, where high-elevation zones have more positive SWE trends. Negative trends are confined to the Himalayan foreland and deeply-incised valleys which run into the Upper Indus. This implies a temperature-dependent cutoff below which precipitation increases are not translated into increased SWE. Earlier snowmelt or a higher percentage of liquid precipitation could both explain this cutoff.(1) Earlier work 2 found a negative snow-water storage trend for the entire Indus catchment over the time period 1987-2009 (-4 x 10(-3) mm/yr). In this study based on an additional seven years of data, the average trend reverses to 1.4 x 10(-3). This implies that the decade since the mid-2000s was likely wetter, and positively impacted long-term SWE trends. This conclusion is supported by an analysis of snowmelt onset and end dates which found that while long-term trends are negative, more recent (since 2005) trends are positive (moving later in the year).(3)
KW  - Passive Microwave
KW  - Snow
KW  - Climate Change
KW  - High Mountain Asia
Y1  - 2018
SN  - 978-1-5106-2160-2
U6  - https://doi.org/10.1117/12.2323827
SN  - 0277-786X
SN  - 1996-756X
VL  - 10788
PB  - SPIE-INT Soc Optical Engineering
CY  - Bellingham
ER  - 
TY  - GEN
A1  - Gudipudi, Venkata Ramana
A1  - Rybski, Diego
A1  - Lüdeke, Matthias K. B.
A1  - Kropp, Jürgen
T1  - Urban emission scaling - Research insights and a way forward
T2  - Environment and Planning B: Urban Analytics and City Science
Y1  - 2019
U6  - https://doi.org/10.1177/2399808319825867
SN  - 2399-8083
SN  - 2399-8091
VL  - 46
IS  - 9
SP  - 1678
EP  - 1683
PB  - Sage Publ.
CY  - London
ER  - 
TY  - GEN
A1  - Lopez-Tarazon, José Andrés
A1  - Byrne, Patrick
A1  - van der Perk, Marcel
T1  - Transfer of Sediments and Contaminants in Catchments and Rivers Preface
T2  - Journal of soils and sediments : protection, risk assessment and remediation
Y1  - 2017
U6  - https://doi.org/10.1007/s11368-017-1810-5
SN  - 1439-0108
SN  - 1614-7480
VL  - 17
SP  - 2577
EP  - 2581
PB  - Springer
CY  - Heidelberg
ER  - 
TY  - GEN
A1  - Geissman, John
A1  - Jolivet, Laurent
A1  - Rusmore, Margi
A1  - Niemi, Nathan
A1  - Schildgen, Taylor F.
T1  - Thank you to our 2018 peer reviewers
T2  - Tectonics
N2  - An essential, respected, and critical aspect of the modern practice of science and scientific publishing is peer review. The process of peer review facilitates best practices in scientific conduct and communication, ensuring that manuscripts published are as accurate, valuable, and clearly communicated. The over 216 papers published in Tectonics in 2018 benefit from the time, effort, and expertise of our reviewers who have provided thoughtfully considered advice on each manuscript. This role is critical to advancing our understanding of the evolution of the continents and their margins, as these reviews lead to even clearer and higher-quality papers. In 2018, the over 443 papers submitted to Tectonics were the beneficiaries of more than 1,010 reviews provided by 668 members of the tectonics community and related disciplines. To everyone who has volunteered their time and intellect to peer reviewing, thank you for helping Tectonics and all other AGU Publications provide the best science possible.
Y1  - 2019
U6  - https://doi.org/10.1029/2019TC005595
SN  - 0278-7407
SN  - 1944-9194
VL  - 38
IS  - 4
SP  - 1159
EP  - 1163
PB  - Hoboken
CY  - Wiley
ER  - 
TY  - GEN
A1  - Geissman, John
A1  - Jolivet, Laurent
A1  - Niemi, Nathan
A1  - Schildgen, Taylor F.
T1  - Thank you to our 2017 Peer Reviewers
T2  - Tectonics
N2  - An essential, respected, and critical aspect of the modern practice of science and scientific publishing is peer review. The process of peer review facilitates best practices in scientific conduct and communication, ensuring that manuscripts published as accurate, valuable, and clearly communicated. The over 152 papers published in Tectonics in 2017 benefit from the time, effort, and expertise of our reviewers who have provided thoughtfully considered advice on each manuscript. This role is critical to advancing our understanding of the evolution of the continents and their margins, as these reviews lead to even clearer and higher-quality papers. In 2017, the over 423 papers submitted to Tectonics were the beneficiaries of more than 786 reviews provided by 562 members of the tectonics community and related disciplines. To everyone who has volunteered their time and intellect to peer reviewing, thank you for helping Tectonics and all other AGU Publications provide the best science possible.
Y1  - 2018
U6  - https://doi.org/10.1029/2018TC005194
SN  - 0278-7407
SN  - 1944-9194
VL  - 37
IS  - 8
SP  - 2272
EP  - 2277
PB  - American Geophysical Union
CY  - Washington
ER  - 
TY  - GEN
A1  - Motagh, Mahdi
T1  - Tectonic and non-tectonic deformation monitoringg using satellite radar interferometry
Y1  - 2007
CY  - Potsdam
ER  - 
TY  - GEN
A1  - Walz, Ariane
A1  - Gret-Regamey, Adrienne
A1  - Lavorel, Sandra
T1  - Social valuation of ecosystem services in mountain regions
T2  - Regional environmental change
Y1  - 2016
U6  - https://doi.org/10.1007/s10113-016-1028-x
SN  - 1436-3798
SN  - 1436-378X
VL  - 16
SP  - 1985
EP  - 1987
PB  - Springer
CY  - Heidelberg
ER  - 
TY  - GEN
A1  - Garcin, Yannick
A1  - Acosta, Veronica Torres
A1  - Melnick, Daniel
A1  - Guillemoteau, Julien
A1  - Willenbring, Jane
A1  - Strecker, Manfred
T1  - Short-lived increase in erosion during the African Humid Period: Evidence from the northern Kenya Rift (vol 759, pg 58, 2017)
T2  - Earth & planetary science letters
Y1  - 2017
U6  - https://doi.org/10.1016/j.epsl.2017.07.027
SN  - 0012-821X
SN  - 1385-013X
VL  - 474
SP  - 528
EP  - 528
PB  - Elsevier
CY  - Amsterdam
ER  - 
TY  - GEN
A1  - Nakaten, Natalie Christine
A1  - Kempka, Thomas
T1  - Retraction: Techno-Economic Comparison of Onshore and Offshore Underground Coal Gasification End-Product Competitiveness. (Retraction of Vol 10, art no 1643, 2017)
T2  - Energies : open-access journal of related scientific research, technology development and studies in policy and management
Y1  - 2019
U6  - https://doi.org/10.3390/en12173253
SN  - 1996-1073
VL  - 12
IS  - 17
PB  - MDPI
CY  - Basel
ER  - 
TY  - GEN
A1  - Braun, Jean
T1  - Response to comment by Japsen et al. on "A review of numerical modeling studies of passive margin escarpments leading to a new analytical expression for the rate of escarpment migration velocity"
T2  - Gondwana research : international geoscience journal ; official journal of the International Association for Gondwana Research
Y1  - 2020
U6  - https://doi.org/10.1016/j.gr.2018.10.003
SN  - 1342-937X
SN  - 1878-0571
VL  - 65
SP  - 174
EP  - 176
PB  - Elsevier
CY  - Amsterdam
ER  - 
TY  - GEN
A1  - Foerster, Verena
A1  - Vogelsang, Ralf
A1  - Junginger, Annett
A1  - Asrat, Asfawossen
A1  - Lamb, Henry F.
A1  - Schäbitz, Frank
A1  - Trauth, Martin H.
T1  - Reply to the comment on "Environmental change and human occupation of southern Ethiopia and northern Kenya during the last 20,000 years. Quaternary Science Reviews 129: 333-340"
T2  - Quaternary science reviews : the international multidisciplinary research and review journal
Y1  - 2016
U6  - https://doi.org/10.1016/j.quascirev.2016.04.003
SN  - 0277-3791
VL  - 141
SP  - 130
EP  - 133
PB  - Elsevier
CY  - Oxford
ER  - 
TY  - GEN
A1  - Braun, David R.
A1  - Aldeias, Vera
A1  - Archer, Will
A1  - Arrowsmith, J. Ramon
A1  - Baraki, Niguss
A1  - Campisano, Christopher J.
A1  - Deino, Alan L.
A1  - DiMaggio, Erin N.
A1  - Dupont-Nivet, Guillaume
A1  - Engda, Blade
A1  - Feary, David A.
A1  - Garello, Dominique I.
A1  - Kerfelew, Zenash
A1  - McPherron, Shannon P.
A1  - Patterson, David B.
A1  - Reeves, Jonathan S.
A1  - Thompson, Jessica C.
A1  - Reed, Kaye E.
T1  - Reply to Sahle and Gossa: Technology and geochronology at the earliest known Oldowan site at Ledi-Geraru, Ethiopia
T2  - Proceedings of the National Academy of Sciences of the United States of America
Y1  - 2019
U6  - https://doi.org/10.1073/pnas.1911952116
SN  - 0027-8424
N1  - Letter
VL  - 116
IS  - 41
SP  - 20261
EP  - 20262
PB  - National Acad. of Sciences
CY  - Washington
ER  - 
TY  - GEN
A1  - Wang, Yongbo
A1  - Herzschuh, Ulrike
A1  - Liu, Xingqi
A1  - Korup, Oliver
A1  - Diekmann, Bernhard
T1  - Reply to Chong Xu’s comment on: Wang, Yongbo; Herzschuh, Ulrike; Liu, Xingqi; Korup, Oliver; Diekmann, Bernhard: A high-resolution sedimentary archive from landslide-dammed Lake Mengda, north-eastern Tibetan Plateau. - Journal of Paleolimnology. -  51 (2014), S. 303 - 312
T2  - Journal of paleolimnolog
Y1  - 2016
U6  - https://doi.org/10.1007/s10933-016-9937-8
SN  - 0921-2728
SN  - 1573-0417
VL  - 57
SP  - 163
EP  - 164
PB  - Springer
CY  - Dordrecht
ER  - 
TY  - GEN
A1  - Dahm, Torsten
A1  - Becker, Dirk
A1  - Bischoff, Monika
A1  - Cesca, Simone
A1  - Dost, B.
A1  - Fritschen, R.
A1  - Hainzl, Sebastian
A1  - Klose, C. D.
A1  - Kuhn, D.
A1  - Lasocki, S.
A1  - Meier, Thomas
A1  - Ohrnberger, Matthias
A1  - Rivalta, Eleonora
A1  - Wegler, Ulrich
A1  - Husen, Stephan
T1  - Recommendation for the discrimination of human-related and natural seismicity
T2  - Journal of seismology
N2  - Various techniques are utilized by the seismological community, extractive industries, energy and geoengineering companies to identify earthquake nucleation processes in close proximity to engineering operation points. These operations may comprise fluid extraction or injections, artificial water reservoir impoundments, open pit and deep mining, deep geothermal power generations or carbon sequestration. In this letter to the editor, we outline several lines of investigation that we suggest to follow to address the discrimination problem between natural seismicity and seismic events induced or triggered by geoengineering activities. These suggestions have been developed by a group of experts during several meetings and workshops, and we feel that their publication as a summary report is helpful for the geoscientific community. Specific investigation procedures and discrimination approaches, on which our recommendations are based, are also published in this Special Issue (SI) of Journal of Seismology.
KW  - Triggered seismicity
KW  - Induced seismicity
Y1  - 2013
U6  - https://doi.org/10.1007/s10950-012-9295-6
SN  - 1383-4649
VL  - 17
IS  - 1
SP  - 197
EP  - 202
PB  - Springer
CY  - Dordrecht
ER  - 
TY  - GEN
A1  - Meere, Patrick A.
A1  - Mulchrone, Kieran F.
A1  - McCarthy, David J.
A1  - Timmerman, Martin Jan
A1  - Dewey, John F.
T1  - Prelithification and synlithification tectonic foliation development in a clastic sedimentary sequence
T2  - Geology
Y1  - 2016
U6  - https://doi.org/10.1130/G38103Y.1
SN  - 0091-7613
SN  - 1943-2682
VL  - 44
SP  - E397
EP  - E397
PB  - American Institute of Physics
CY  - Boulder
ER  - 
TY  - GEN
A1  - Bubeck, Philip
A1  - Aerts, Jeroen C. J. H.
A1  - de Moel, Hans
A1  - Kreibich, Heidi
T1  - Preface: Flood-risk analysis and integrated management
T2  - Natural hazards and earth system sciences
Y1  - 2016
U6  - https://doi.org/10.5194/nhess-16-1005-2016
SN  - 1561-8633
VL  - 16
SP  - 1005
EP  - 1010
PB  - Copernicus
CY  - Göttingen
ER  - 
TY  - GEN
A1  - Lühr, Hermann
A1  - Wicht, Johannes
A1  - Gilder, Stuart A.
A1  - Holschneider, Matthias
T1  - Preface
T2  - Magnetic Fields in the Solar System: Planets, Moons and Solar Wind Interactions
Y1  - 2018
SN  - 978-3-319-64292-5
SN  - 978-3-319-64291-8
SN  - 0067-0057
VL  - 448
SP  - V
EP  - VI
PB  - Springer
CY  - Dordrecht
ER  - 
TY  - GEN
A1  - Wetzel, Maria
A1  - Kempka, Thomas
A1  - Kühn, Michael
T1  - Predicting macroscopic elastic rock properties requires detailed information on microstructure
T2  - Energy procedia
N2  - Predicting variations in macroscopic mechanical rock behaviour due to microstructural changes, driven by mineral precipitation and dissolution is necessary to couple chemo-mechanical processes in geological subsurface simulations. We apply 3D numerical homogenization models to estimate Young’s moduli for five synthetic microstructures, and successfully validate our results for comparable geometries with the analytical Mori-Tanaka approach. Further, we demonstrate that considering specific rock microstructures is of paramount importance, since calculated elastic properties may deviate by up to 230 % for the same mineral composition. Moreover, agreement between simulated and experimentally determined Young’s moduli is significantly improved, when detailed spatial information are employed.
KW  - digital rock physics
KW  - effective elastic properties
KW  - numerical
Y1  - 2017
U6  - https://doi.org/10.1016/j.egypro.2017.08.195
SN  - 1876-6102
VL  - 125
SP  - 561
EP  - 570
PB  - Elsevier
CY  - Amsterdam
ER  - 
TY  - GEN
A1  - Hoehnel, Desiree
A1  - Reimold, W. U.
A1  - Mohr-Westheide, Tanja
A1  - Hofmann, Axel
A1  - Altenberger, Uwe
T1  - PETROGRAPHY OF ARCHEAN SPHERULE LAYERS FROM THE CT3 DRILL CORE, BARBERTON GREENSTONE BELT, SOUTH AFRICA
T2  - Scientific reports
Y1  - 2016
SN  - 1086-9379
SN  - 1945-5100
VL  - 51
SP  - A333
EP  - A333
PB  - Wiley-Blackwell
CY  - Hoboken
ER  - 
TY  - GEN
A1  - Sprinz, Detlef F.
ED  - Luterbacher, Urs
ED  - Sprinz, Detlef F.
T1  - Our Conclusions
T2  - Global Climate Policy: Actors, Concepts, and Enduring Challenges
Y1  - 2018
SN  - 978-0-262-53534-2
SN  - 978-0-262-03792-1
SP  - 323
EP  - 335
PB  - MIT Press
CY  - Cambridge
ER  - 
TY  - GEN
A1  - Voropaev, S.
A1  - Korochantsev, A.
A1  - Petukhov, D.
A1  - Kocherov, A.
A1  - Kaeter, David
A1  - Ziemann, Martin Andreas
A1  - Boettger, Ute
T1  - Ordinary chondrites of Chelyabinsk meteorite and comparison with asteroid 25143 (Itokawa)
T2  - PLoS one
Y1  - 2016
SN  - 1086-9379
SN  - 1945-5100
VL  - 51
SP  - A644
EP  - A644
PB  - Wiley-Blackwell
CY  - Hoboken
ER  - 
TY  - GEN
A1  - Rounsevell, Mark D. A.
A1  - Metzger, Marc J.
A1  - Walz, Ariane
T1  - Operationalising ecosystem services in Europe
T2  - Regional environmental change
Y1  - 2019
U6  - https://doi.org/10.1007/s10113-019-01560-1
SN  - 1436-3798
SN  - 1436-378X
VL  - 19
IS  - 8
SP  - 2143
EP  - 2149
PB  - Springer
CY  - Heidelberg
ER  - 
TY  - GEN
A1  - Garcin, Yannick
A1  - Deschamps, Pierre
A1  - Menot, Guillemette
A1  - de Saulieu, Geoffroy
A1  - Schefuss, Enno
A1  - Sebag, David
A1  - Dupont, Lydie M.
A1  - Oslisly, Richard
A1  - Brademann, Brian
A1  - Mbusnum, Kevin G.
A1  - Onana, Jean-Michel
A1  - Ako, Andrew A.
A1  - Epp, Laura Saskia
A1  - Tjallingii, Rik
A1  - Strecker, Manfred
A1  - Brauer, Achim
A1  - Sachse, Dirk
T1  - No evidence for climate variability during the late Holocene rainforest crisis in Western Central Africa REPLY
T2  - Proceedings of the National Academy of Sciences of the United States of America
Y1  - 2018
U6  - https://doi.org/10.1073/pnas.1808481115
SN  - 0027-8424
VL  - 115
IS  - 29
SP  - E6674
EP  - E6675
PB  - National Acad. of Sciences
CY  - Washington
ER  - 
TY  - GEN
A1  - Rheinwalt, Aljoscha
A1  - Bookhagen, Bodo
T1  - Network-based flow accumulation for point clouds
BT  - Facet-Flow Networks (FFN)
T2  - Remote Sensing for Agriculture, Ecosystems, and Hydrology XX
N2  - Point clouds provide high-resolution topographic data which is often classified into bare-earth, vegetation, and building points and then filtered and aggregated to gridded Digital Elevation Models (DEMs) or Digital Terrain Models (DTMs). Based on these equally-spaced grids flow-accumulation algorithms are applied to describe the hydrologic and geomorphologic mass transport on the surface. In this contribution, we propose a stochastic point-cloud filtering that, together with a spatial bootstrap sampling, allows for a flow accumulation directly on point clouds using Facet-Flow Networks (FFN). Additionally, this provides a framework for the quantification of uncertainties in point-cloud derived metrics such as Specific Catchment Area (SCA) even though the flow accumulation itself is deterministic.
KW  - lidar
KW  - point clouds
KW  - stochastic filtering
KW  - flow accumulation
KW  - drainage networks
KW  - uncertainty quantification
KW  - TIN
KW  - DEM
Y1  - 2018
SN  - 978-1-5106-2150-3
U6  - https://doi.org/10.1117/12.2318424
SN  - 0277-786X
SN  - 1996-756X
VL  - 10783
PB  - SPIE-INT  Society of Photo-Optical Instrumentation Engineers
CY  - Bellingham
ER  - 
TY  - GEN
A1  - Kühn, Michael
A1  - Schöne, Tim
T1  - Multivariate regression model from water level and production rate time series for the geothermal reservoir Waiwera (New Zealand)
T2  - Energy procedia
N2  - Water management tools are necessary to guarantee the preservation of natural resources while ensuring optimum utilization. Linear regression models are a simple and quick solution for creating prognostic capabilities. Multivariate models show higher precision than univariate models. In the case of Waiwera, implementation of individual production rates is more accurate than applying just the total production rate. A maximum of approximately 1,075 m3/day can be pumped to ensure a water level of at least 0.5 m a.s.l. in the monitoring well. The model should be renewed annually to implement new data and current water level trends to keep the quality.
KW  - geothermal reservoir
KW  - water management
KW  - data based model
KW  - multivariate regression
KW  - coefficient of determination
KW  - scenario analysis
Y1  - 2017
U6  - https://doi.org/10.1016/j.egypro.2017.08.196
SN  - 1876-6102
VL  - 125
SP  - 571
EP  - 579
PB  - Elsevier
CY  - Amsterdam
ER  - 
TY  - GEN
A1  - Wagner, Kathrin
A1  - Oswald, Sascha
A1  - Frick, Annett
T1  - Multitemporal soil moisture monitoring by use of optical remote sensing data in a dike relocation area
T2  - Remote Sensing for Agriculture, Ecosystems, and Hydrology XX
N2  - The nature restoration project ‘Lenzener Elbtalaue’, realised from 2002 to 2011 at the river Elbe, included the first large scale dike relocation in Germany (420 ha). Its aim was to initiate the development of endangered natural wetland habitats and processes, accompanied by greater biodiversity in the former grassland dominated area. The monitoring of spatial and temporal variations of soil moisture in this dike relocation area is therefore particularly important for estimating the restoration success. The topsoil moisture monitoring from 1990 to 2017 is based on the Soil Moisture Index (SMI)1 derived with the triangle method2 by use of optical remotely sensed data: land surface temperature and Normalized Differnce Vegetation Index are calculated from Landsat 4/5/7/8 data and atmospheric corrected by use of MODIS data. Spatial and temporal soil moisture variations in the restored area of the dike relocation are compared to the agricultural and pasture area behind the new dike. Ground truth data in the dike relocation area was obtained from field measurements in October 2017 with a FDR device. Additionally, data from a TERENO soil moisture sensor network (SoilNet) and mobile cosmic ray neutron sensing (CRNS) rover measurements are compared to the results of the triangle method for a region in the Harz Mountains (Germany). The SMI time series illustrates, that the dike relocation area has become significantly wetter between 1990 and 2017, due to restructuring measurements. Whereas the SMI of the dike hinterland reflects constant and drier conditions. An influence of climate is unlikely. However, validation of the dimensionless index with ground truth measurements is very difficult, mostly due to large differences in scale.
KW  - soil moisture
KW  - time series
KW  - SMI
KW  - triangle method
KW  - Landsat
KW  - restoration
Y1  - 2018
SN  - 978-1-5106-2150-3
U6  - https://doi.org/10.1117/12.2325319
SN  - 0277-786X
SN  - 1996-756X
VL  - 10783
PB  - SPIE-INT Soc Optical Engineering
CY  - Bellingham
ER  - 
TY  - GEN
A1  - Mangili, Clara
T1  - Microfacies and isotope analyses of the varved Piànico lake sediment profile for high-resolution reconstruction of interglacial climate dynamics
Y1  - 2006
CY  - Potsdam
ER  - 
TY  - GEN
A1  - Hoehnel, Desirée
A1  - Tagle, Roald
A1  - Hofmann, Axel
A1  - Reimold, W. U.
A1  - Mohr-Westheide, Tanja
A1  - Fritz, Joerg
A1  - Altenberger, Uwe
T1  - MICRO-XRF ANALYSIS OF ARCHEAN SPHERULE LAYERS AND HOST ROCKS FROM THE CT3 DRILL CORE, BARBERTON GREENSTONE BELT, SOUTH AFRICA
T2  - Monthly notices of the Royal Astronomical Society
Y1  - 2016
SN  - 1086-9379
SN  - 1945-5100
VL  - 51
SP  - A334
EP  - A334
PB  - Wiley-Blackwell
CY  - Hoboken
ER  - 
TY  - GEN
A1  - Bobos, Iuliu
A1  - Goncalves, Ana
A1  - Lima, Luis
A1  - Noronha, Fernando
A1  - Sudo, Masafumi
T1  - Micas Ar-40/Ar-39 dating of hydrothermal events related with the post-orogenic W (+/- Sn), (Cu, Mo) mineralization from Borralha, Northern Portugal
T2  - Life with Ore Deposits on Earth – 15th SGA Biennial Meeting 2019,
N2  - Secondary mica minerals collected from the Santa Helena (W- (Cu) mineralization) and Venise (W-Mo mineralization) endogenic breccia structures were Ar-40/Ar-39 dated. The muscovite Ar-40/Ar-39 data yielded 286.8 +/- 1.2 (+/- 1 sigma) Ma (samples 6Ha and 11Ha) which reflect the age of secondary muscovite formation probably from magmatic biotite or feldspar alteration. Sericite Ar-40/Ar-39 data yielded 280.9 +/- 1.2 (+/- 1 sigma) Ma to 279.0 +/- 1.1 (+/- 1 sigma) Ma (samples 6Hb and 11Hb) reflecting the age of greisen alteration (T similar to 300 degrees C) where the W- disseminated mineralization occurs. The muscovite 40Ar/39Ar data of 277.3 +/- 1.3 (+/- 1 sigma) Ma and 281.3 +/- 1.2 (+/- 1 sigma) Ma (samples 5 and 6) also reflect the age of muscovite (selvage) crystallized adjacent to molybdenite veins within the Venise breccia. Geochronological data obtained confirmed that the W mineralization at Santa Helena breccia is older than Mo-mineralization at Venise breccia. Also, the timing of hydrothermal circulation and the cooling history for the W-stage deposition was no longer than 7 Ma and 4 Ma for Mo-deposition.
Y1  - 2019
UR  - https://www.researchgate.net/publication/337901420_Micas_40_Ar_39_Ar_dating_of_hydrothermal_events_related_with_the_post-orogenic_W_Sn_Cu_Mo_mineralization_from_Borralha_Northern_Portugal
IS  - 1
SP  - 353
EP  - 356
PB  - SGA Soc Geology Applied mineral  depositis
CY  - Geneva
ER  - 
TY  - GEN
A1  - Thiede, Rasmus Christoph
A1  - Ehlers, Todd
T1  - Large spatial and temporal variations in Himalayan denudation (vol 371, pg 278, 2013)
T2  - Earth & planetary science letters
Y1  - 2013
U6  - https://doi.org/10.1016/j.epsl.2013.07.004
SN  - 0012-821X
VL  - 374
IS  - 13
SP  - 256
EP  - 257
PB  - Elsevier
CY  - Amsterdam
ER  - 
TY  - GEN
A1  - Duydu, Yalcin
A1  - Basaran, Nursen
A1  - Aydin, Sevtap
A1  - Ustundag, Aylin
A1  - Goktas, Hatica Gul
A1  - Yalcin, Can Özgür
A1  - Bacanli, Merve
A1  - Sarigol, Zehra
A1  - Aydos, Kaan
A1  - Atabekoglu, Cem Somer
A1  - Schwerdtle, Tanja
A1  - Golka, Klaus
A1  - Ickstadt, Katja
A1  - Bolt, Hermann M.
T1  - Investigation of boron mediated reproductive and developmental effects in highly boron exposed population
T2  - Toxicology letters
Y1  - 2017
U6  - https://doi.org/10.1016/j.toxlet.2017.07.259
SN  - 0378-4274
SN  - 1879-3169
VL  - 280
SP  - S94
EP  - S94
PB  - Elsevier
CY  - Clare
ER  - 
TY  - GEN
A1  - Kühn, Michael
A1  - Li, Qi
A1  - Nakaten, Natalie Christine
A1  - Kempka, Thomas
T1  - Integrated subsurface gas storage of CO2 and CH4 offers capacity and state-of-the-art technology for energy storage in China
T2  - Energy procedia
N2  - Integration and development of the energy supply in China and worldwide is a challenge for the years to come. The innovative idea presented here is based on an extension of the “power-to-gas-to-power” technology by establishing a closed carbon cycle. It is an implementation of a low-carbon energy system based on carbon dioxide capture and storage (CCS) to store and reuse wind and solar energy. The Chenjiacun storage project in China compares well with the German case study for the towns Potsdam and Brandenburg/Havel in the Federal State of Brandenburg based on the Ketzin pilot site for CCS.
KW  - gas storage
KW  - carbon dioxide
KW  - methane
KW  - hydrogen
KW  - renewable energy
KW  - carbon cycle
Y1  - 2017
U6  - https://doi.org/10.1016/j.egypro.2017.08.039
SN  - 1876-6102
VL  - 125
SP  - 14
EP  - 18
PB  - Elsevier
CY  - Amsterdam
ER  - 
TY  - GEN
A1  - Lehmann, Jascha
A1  - Coumou, Dim
A1  - Frieler, Katja
T1  - Increased record-breaking precipitation events under global warming (vol 132, pg 501, 2015)
T2  - Climatic change : an interdisciplinary, intern. journal devoted to the description, causes and implications of climatic change
Y1  - 2015
U6  - https://doi.org/10.1007/s10584-015-1466-3
SN  - 0165-0009
SN  - 1573-1480
VL  - 132
IS  - 4
SP  - 517
EP  - 518
PB  - Springer
CY  - Dordrecht
ER  - 
TY  - GEN
A1  - Garcin, Yannick
A1  - Deschamps, Pierre
A1  - Menot, Guillemette
A1  - de Saulieu, Geoffroy
A1  - Schefuss, Enno
A1  - Sebag, David
A1  - Dupont, Lydie M.
A1  - Oslisly, Richard
A1  - Brademann, Brian
A1  - Mbusnum, Kevin G.
A1  - Onana, Jean-Michel
A1  - Ako, Andrew A.
A1  - Epp, Laura Saskia
A1  - Tjallingii, Rik
A1  - Strecker, Manfred
A1  - Brauer, Achim
A1  - Sachse, Dirk
T1  - Human activity is the most probable trigger of the late Holocene rainforest crisis in Western Central Africa Reply
T2  - Proceedings of the National Academy of Sciences of the United States of America
Y1  - 2018
U6  - https://doi.org/10.1073/pnas.1805582115
SN  - 0027-8424
VL  - 115
IS  - 21
SP  - E4735
EP  - E4736
PB  - National Acad. of Sciences
CY  - Washington
ER  - 
TY  - GEN
A1  - Hugenschmidt, Johannes
A1  - Giannopoulos, Antonios
A1  - Tronicke, Jens
T1  - Foreword
T2  - Near surface geophysics
Y1  - 2019
U6  - https://doi.org/10.1002/nsg.12050
SN  - 1569-4445
SN  - 1873-0604
VL  - 17
IS  - 3
SP  - 199
EP  - 200
PB  - Wiley
CY  - Oxford
ER  - 
TY  - GEN
A1  - Luterbacher, Urs
A1  - Sprinz, Detlef F.
ED  - Luterbacher, Urs
ED  - Sprinz, Detlef F.
T1  - Foreword
T2  - Global climate policy: actors, concepts, and enduring challenges
Y1  - 2018
SN  - 978-0-262-53534-2
SN  - 978-0-262-03792-1
SP  - IX
EP  - XI
PB  - MIT Press
CY  - Cambridge
ER  - 
TY  - GEN
A1  - Brune, Sascha
T1  - Forces within continental and oceanic rifts
BT  - numerical modeling elucidates the impact of asthenospheric flow on surface stress
T2  - Geology
Y1  - 2018
U6  - https://doi.org/10.1130/focus022018.1
SN  - 0091-7613
SN  - 1943-2682
VL  - 46
IS  - 2
SP  - 191
EP  - 192
PB  - American Institute of Physics
CY  - Boulder
ER  - 
TY  - GEN
A1  - Sommer, Michael
A1  - Augustin, Jürgen
A1  - Kleber, M.
T1  - Feedbacks of soil erosion on SOC patterns and carbon dynamics in agricultural landscapes-The CarboZALF experiment
T2  - Journal of real-time image processing
Y1  - 2016
U6  - https://doi.org/10.1016/j.still.2015.09.015
SN  - 0167-1987
SN  - 1879-3444
VL  - 156
SP  - 182
EP  - 184
PB  - Elsevier
CY  - Amsterdam
ER  - 
TY  - GEN
A1  - Bousquet, Romain
A1  - De Capitani, Christian
A1  - Arcay, Diane
T1  - Feedback of the metamorphic changes on the subducting processes
T2  - Geochimica et cosmochimica acta : journal of the Geochemical Society and the Meteoritical Society
Y1  - 2006
U6  - https://doi.org/10.1016/j.gca.2006.06.228
SN  - 0016-7037
VL  - 70
IS  - 18
SP  - A62
EP  - A62
PB  - Elsevier
CY  - Oxford
ER  - 
TY  - GEN
A1  - Radosavljevic, Boris
A1  - Lantuit, Hugues
A1  - Pollard, Wayne
A1  - Overduin, Pier Paul
A1  - Couture, Nicole
A1  - Sachs, Torsten
A1  - Helm, Veit
A1  - Fritz, Michael
T1  - Erosion and Flooding - Threats to Coastal Infrastructure in the Arctic: A Case Study from Herschel Island, Yukon Territory, Canada (vol 39, pg 900, 2016)
T2  - Estuaries and coasts : journal of the Estuarine Research Federation
Y1  - 2016
U6  - https://doi.org/10.1007/s12237-016-0115-z
SN  - 1559-2723
SN  - 1559-2731
VL  - 39
SP  - 1294
EP  - 1295
PB  - Springer
CY  - New York
ER  - 
TY  - GEN
A1  - Mischke, Steffen
A1  - Zhang, Chengjun
A1  - Fan, Rong
T1  - Early to mid-Holocene lake high-stand sediments at Lake Donggi Cona, northeastern Tibetan Plateau, China -
T2  - Quaternary research : an interdisciplinary journal
KW  - Microfossils
KW  - Ostracoda
KW  - Lake level
KW  - Wetlands
KW  - Depositional setting
KW  - Tibetan Plateau
KW  - Holocene
Y1  - 2015
U6  - https://doi.org/10.1016/j.yqres.2014.06.005
SN  - 0033-5894
SN  - 1096-0287
VL  - 83
IS  - 1
SP  - 256
EP  - 258
PB  - Elsevier
CY  - San Diego
ER  - 
TY  - GEN
A1  - Mirus, Benjamin B.
A1  - Ebel, Brian A.
A1  - Mohr, Christian Heinrich
A1  - Zegre, Nicolas
T1  - Disturbance Hydrology: Preparing for an Increasingly Disturbed Future
T2  - Water resources research
N2  - This special issue is the result of several fruitful conference sessions on disturbance hydrology, which started at the 2013 AGU Fall Meeting in San Francisco and have continued every year since. The stimulating presentations and discussions surrounding those sessions have focused on understanding both the disruption of hydrologic functioning following discrete disturbances, as well as the subsequent recovery or change within the affected watershed system. Whereas some hydrologic disturbances are directly linked to anthropogenic activities, such as resource extraction, the contributions to this special issue focus primarily on those with indirect or less pronounced human involvement, such as bark-beetle infestation, wildfire, and other natural hazards. However, human activities are enhancing the severity and frequency of these seemingly natural disturbances, thereby contributing to acute hydrologic problems and hazards. Major research challenges for our increasingly disturbed planet include the lack of continuous pre and postdisturbance monitoring, hydrologic impacts that vary spatially and temporally based on environmental and hydroclimatic conditions, and the preponderance of overlapping or compounding disturbance sequences. In addition, a conceptual framework for characterizing commonalities and differences among hydrologic disturbances is still in its infancy. In this introduction to the special issue, we advance the fusion of concepts and terminology from ecology and hydrology to begin filling this gap. We briefly explore some preliminary approaches for comparing different disturbances and their hydrologic impacts, which provides a starting point for further dialogue and research progress.
Y1  - 2017
U6  - https://doi.org/10.1002/2017WR021084
SN  - 0043-1397
SN  - 1944-7973
VL  - 53
SP  - 10007
EP  - 10016
PB  - American Geophysical Union
CY  - Washington
ER  - 
TY  - GEN
A1  - Kühn, Michael
A1  - Kempka, Thomas
A1  - de Lucia, Marco
A1  - Scheck-Wenderoth, Magdalena
T1  - Dissolved CO2 storage in geological formations with low pressure, low risk and large capacities
T2  - Energy procedia
N2  - Geological CO2 storage is a mitigation technology to reduce CO2 emissions from fossil fuel combustion. However, major concerns are the pressure increase and saltwater displacement in the mainly targeted deep groundwater aquifers due to injection of supercritical CO2. The suggested solution is storage of CO2 exclusively in the dissolved state. In our exemplary regional case study of the North East German Basin based on a highly resolved temperature and pressure distribution model and a newly developed reactive transport coupling, we have quantified that 4.7 Gt of CO2 can be stored in solution compared to 1.5 Gt in the supercritical state.
KW  - carbon dioxide
KW  - dissolved
KW  - storage capacity
KW  - numerical simulation
KW  - saline aquifer
KW  - Buntsandstein
Y1  - 2017
U6  - https://doi.org/10.1016/j.egypro.2017.03.1607
SN  - 1876-6102
VL  - 114
SP  - 4722
EP  - 4727
PB  - Elsevier
CY  - Amsterdam
ER  - 
TY  - GEN
A1  - Shprits, Yuri Y.
A1  - Zhelavskaya, Irina
A1  - Green, Janet C.
A1  - Pulkkinen, Antti A.
A1  - Horne, Richard B.
A1  - Pitchford, David
A1  - Glover, Alexi
T1  - Discussions on Stakeholder Requirements for Space Weather-Related Models
T2  - Space Weather: The International Journal of Research and Applications
N2  - Participants of the 2017 European Space Weather Week in Ostend, Belgium, discussed the stakeholder requirements for space weather-related models. It was emphasized that stakeholders show an increased interest in space weather-related models. Participants of the meeting discussed particular prediction indicators that can provide first-order estimates of the impact of space weather on engineering systems.
KW  - 7924
KW  - 7934
KW  - 7959
Y1  - 2018
U6  - https://doi.org/10.1002/2018SW001864
SN  - 1542-7390
VL  - 16
IS  - 4
SP  - 341
EP  - 342
PB  - American Geophysical Union
CY  - Washington
ER  - 
TY  - GEN
A1  - Wawrzenitz, Nicole
A1  - Krohe, Alexander
T1  - Deformed monazite yields high-temperature tectonic ages
T2  - Geology
Y1  - 2016
U6  - https://doi.org/10.1130/G37394C.1
SN  - 0091-7613
SN  - 1943-2682
VL  - 44
SP  - E377
EP  - E377
PB  - American Institute of Physics
CY  - Boulder
ER  - 
TY  - GEN
A1  - Ayzel, Georgy
A1  - Izhitskiy, Alexander
ED  - Xu, Z Peng
T1  - Coupling physically based and data-driven models for assessing freshwater inflow into the Small Aral Sea
T2  - Innovative Water Resources Management in a Changing Environment – Understanding and Balancing Interactions between Humankind and Nature
N2  - The Aral Sea desiccation and related changes in hydroclimatic conditions on a regional level is a hot topic for past decades. The key problem of scientific research projects devoted to an investigation of modern Aral Sea basin hydrological regime is its discontinuous nature - the only limited amount of papers takes into account the complex runoff formation system entirely. Addressing this challenge we have developed a continuous prediction system for assessing freshwater inflow into the Small Aral Sea based on coupling stack of hydrological and data-driven models. Results show a good prediction skill and approve the possibility to develop a valuable water assessment tool which utilizes the power of classical physically based and modern machine learning models both for territories with complex water management system and strong water-related data scarcity. The source code and data of the proposed system is available on a Github page (https://github.com/SMASHIproject/IWRM2018).
Y1  - 2018
U6  - https://doi.org/10.5194/piahs-379-151-2018
SN  - 2199-899X
VL  - 379
SP  - 151
EP  - 158
PB  - Copernicus
CY  - Göttingen
ER  - 
TY  - GEN
A1  - Jara, Jorge
A1  - Sánchez-Reyes, Hugo
A1  - Socquet, Anne
A1  - Cotton, Fabrice
A1  - Virieux, Jean
A1  - Maksymowicz, Andrei
A1  - Díaz-Mojica, John
A1  - Walpersdorf, Andrea
A1  - Ruiz, Javier
A1  - Cotte, Nathalie
A1  - Norabuena, Edmundo
T1  - Corrigendum to: Kinematic study of Iquique 2014 Mw 8.1 earthquake: Understanding the segmentation of the seismogenic zone. - (Earth and planetary science letters. - 503 (2018) S. 131 – 143)
T2  - Earth and planetary science letters
N2  - We study the rupture processes of Iquique earthquake 8.1 (2014/04/01) and its largest aftershock 7.7 (2014/04/03) that ruptured the North Chile subduction zone. High-rate Global Positioning System (GPS) recordings and strong motion data are used to reconstruct the evolution of the slip amplitude, rise time and rupture time of both earthquakes. A two-step inversion scheme is assumed, by first building prior models for both earthquakes from the inversion of the estimated static displacements and then, kinematic inversions in the frequency domain are carried out taken into account this prior information. The preferred model for the mainshock exhibits a seismic moment of 1.73 × 1021 Nm ( 8.1) and maximum slip of ∼9 m, while the aftershock model has a seismic moment of 3.88 × 1020 ( 7.7) and a maximum slip of ∼3 m. For both earthquakes, the final slip distributions show two asperities (a shallow one and a deep one) separated by an area with significant slip deficit. This suggests a segmentation along-dip which might be related to a change of the dipping angle of the subducting slab inferred from gravimetric data. Along-strike, the areas where the seismic ruptures stopped seem to be well correlated with geological features observed from geophysical information (high-resolution bathymetry, gravimetry and coupling maps) that are representative of the long-term segmentation of the subduction margin. Considering the spatially limited portions that were broken by these two earthquakes, our results support the idea that the seismic gap is not filled yet.
Y1  - 2018
U6  - https://doi.org/10.1016/j.epsl.2018.11.026
SN  - 0012-821X
SN  - 1385-013X
VL  - 506
SP  - 347
EP  - 347
PB  - Elsevier
CY  - Amsterdam
ER  -