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Res., 46, 10.1029\u002F2008WR007082",{"doi":792},"10.1029\u002F2008WR007082",{"id":24,"text":794,"url":24,"identifiers":795},"Peel, 2007, Updated world map of the Köppen-Geiger climate classification, Hydrol. Earth Syst. Sci., 11, 1633, 10.5194\u002Fhess-11-1633-2007",{"doi":796},"10.5194\u002Fhess-11-1633-2007",{"id":24,"text":798,"url":24,"identifiers":799},"Pielke, 2001, Influence of the spatial distribution of vegetation and soils on the prediction of cumulus convective rainfall, Rev. Geophys., 39, 151, 10.1029\u002F1999RG000072",{"doi":800},"10.1029\u002F1999RG000072",{"id":24,"text":802,"url":24,"identifiers":803},"Pielke, 2009, Climate change: The need to consider human forcings besides greenhouse gases, Eos Trans. AGU, 90, 10.1029\u002F2009EO450008",{"doi":804},"10.1029\u002F2009EO450008",{"id":24,"text":806,"url":24,"identifiers":807},"Shibuo, 2007, Hydrological responses to climate change and irrigation in the Aral Sea drainage basin, Geophys. Res. Lett., 34, 10.1029\u002F2007GL031465",{"doi":808},"10.1029\u002F2007GL031465",{"id":24,"text":810,"url":24,"identifiers":811},"Takata, 2009, Changes in the Asian monsoon climate during 1700-1850 induced by preindustrial cultivation, Proc. Natl. Acad. Sci. U. S. A., 106, 9586, 10.1073\u002Fpnas.0807346106",{"doi":812},"10.1073\u002Fpnas.0807346106",{"id":24,"text":814,"url":24,"identifiers":815},"Villarini, 2009, Flood frequency analysis for nonstationary annual peak records in an urban drainage basin, Adv. Water Resour., 32, 1255, 10.1016\u002Fj.advwatres.2009.05.003",{"doi":816},"10.1016\u002Fj.advwatres.2009.05.003",{"id":24,"text":818,"url":24,"identifiers":819},"World Commission on Dams 2000 Dams and development: A new framework for decision-making Earthscan London http:\u002F\u002Fwww.dams.org\u002Fpublications\u002F",{"doi":820},"10.1108\u002Femh.2001.12.4.444.2",{"id":822,"createTime":823,"updateTime":823,"relativeEntities":824,"slug":825,"properties":826,"entityType":228,"verifyStatus":229,"verifyTime":823,"verifyNote":231,"syncStatus":23,"languages":838,"translateLanguages":24,"viewCount":25,"primaryUrl":839,"fullTextUrl":24,"authors":840,"publicationType":275,"publisherRelationship":900,"citationCount":936,"citationInfo":937,"publishDate":939,"publishYear":940,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":24,"openAccess":24,"references":941,"isForceReanalyzing":373},"1dd6671e-33da-4148-8dda-6726e30f5e98","2025-01-23T23:36:42.343+00:00",[],"Impact-of-nesting-strategies-in-dynamical-downscaling-of-reanalysis-data",{"mag":827,"keywords":829,"openalex":830,"abstract":832,"title":834,"doi":836},{"VOID":828},"2013630901",{},{"VOID":831},"W2013630901",{"EN":833},"\u003Cjats:p>Coarse–grid global numerical weather simulations or analysis data have to be downscaled, e.g., with nested limited–area models (LAMs), for regional interpretation. Here, the impact of different one–way nesting strategies on precipitation simulations over the European Alps with the LAM ALADIN is studied. The LAM is forced by initial and lateral boundary data derived from ERA40 reanalyses with 120 km horizontal gridspacing and 6 h update interval. The nesting strategies considered include relaxation–based techniques with direct nesting of the high–resolution LAM (horizontal gridspacing Δx = 12 km; domain size 2800 × 2500 km\u003Cjats:sup>2\u003C\u002Fjats:sup>) or double nesting with an intermediate–resolution nest (Δx = 50 km). Additionally, the impact of a spectral initialization technique is investigated. Results indicate that the considered nesting strategies are comparably successful in terms of precipitation simulation, despite the large resolution jump (120 to 12 km) involved. Thus, the cheapest method in terms of computational resources, i.e., direct nesting, seems to be the most adequate for dynamical downscaling of reanalysis data over complex terrain.\u003C\u002Fjats:p>",{"EN":835},"Impact of nesting strategies in dynamical downscaling of reanalysis data",{"VOID":837},"10.1029\u002F2004gl020115",[233],"https:\u002F\u002Fagupubs.onlinelibrary.wiley.com\u002Fdoi\u002F10.1029\u002F2004GL020115",[841,861,883],{"id":842,"sortIndex":124,"researcher":24,"roles":843,"affiliations":844,"properties":856},"bef0e564-0be8-4856-838f-8dda627e42bb",[],[845],{"id":846,"sortIndex":25,"affiliation":847,"properties":24},"4d00908f-9171-4289-a303-59c8b9323781",{"id":848,"createTime":849,"updateTime":850,"relativeEntities":851,"slug":852,"properties":853,"entityType":53,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},"2ca0d3b3-07e9-4ec1-bf59-bfdc17e95ccd","2024-01-28T07:02:46.746+00:00","2025-01-23T23:36:42.405+00:00",[],"Central-Institute-of-Meteorology-and-Geodynamics-Vienna-Austria",{"title":854},{"VI":855},"Central Institute of Meteorology and Geodynamics, Vienna, Austria",{"openalex":857,"title":859},{"VOID":858},"A5045410164",{"EN":860},"K. 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Soc., 56, 527",{},{"id":24,"text":976,"url":24,"identifiers":977},"Steinacker R., 2000, The “MAP–SOP MAN,”, MAP Newsl., 12, 2",{},{"id":24,"text":979,"url":24,"identifiers":980},"10.1175\u002F1520-0493(2000)128\u003C3664:ASNTFD>2.0.CO;2",{"doi":979},{"id":24,"text":982,"url":24,"identifiers":983},"10.1175\u002F1520-0477(1997)078\u003C2599:ATOLBC>2.0.CO;2",{"doi":982},{"id":985,"createTime":986,"updateTime":986,"relativeEntities":987,"slug":988,"properties":989,"entityType":228,"verifyStatus":229,"verifyTime":986,"verifyNote":231,"syncStatus":23,"languages":1001,"translateLanguages":24,"viewCount":25,"primaryUrl":1002,"fullTextUrl":24,"authors":1003,"publicationType":275,"publisherRelationship":1193,"citationCount":1229,"citationInfo":1230,"publishDate":1235,"publishYear":1236,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":24,"openAccess":24,"references":1237,"isForceReanalyzing":373},"317d35b0-95aa-4ec1-9b91-5583aa1660ca","2024-09-04T23:36:16.658+00:00",[],"Dam-Construction-in-Lancang-Mekong-River-Basin-Could-Mitigate-Future-Flood-Risk-From-Warming-Induced-Intensified-Rainfall",{"mag":990,"keywords":992,"openalex":993,"abstract":995,"title":997,"doi":999},{"VOID":991},"2761093263",{},{"VOID":994},"W2761093263",{"EN":996},"\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>Water resources management, in particular flood control, in the Lancang‐Mekong River Basin (LMRB) faces two key challenges in the 21st century: climate change and dam construction. A large‐scale distributed Geomorphology‐Based Hydrological Model coupled with a simple reservoir regulation model (GBHM‐LMK‐SOP) is used to investigate the relative effects of climate change and dam construction on the flood characteristics in the LMRB. Results suggest an increase in both flood magnitude and frequency under climate change, which is more severe in the upstream basin and increases over time. However, stream regulation by dam reduces flood risk consistently throughout this century, with more obvious effects in the upstream basin where larger reservoirs will be located. The flood mitigation effect of dam regulation dominates over the flood intensification effect of climate change before 2060, but the latter emerges more prominently after 2060 and dominates the flood risk especially in the lower basin.\u003C\u002Fjats:p>",{"EN":998},"Dam Construction in Lancang‐Mekong River Basin Could Mitigate Future Flood Risk From Warming‐Induced Intensified Rainfall",{"VOID":1000},"10.1002\u002F2017gl075037",[233],"https:\u002F\u002Fagupubs.onlinelibrary.wiley.com\u002Fdoi\u002F10.1002\u002F2017GL075037",[1004,1023,1045,1078,1100,1125,1153,1176],{"id":1005,"sortIndex":129,"researcher":24,"roles":1006,"affiliations":1007,"properties":1018},"14d56493-5f0a-4a0e-a5ca-66cada1fef16",[],[1008],{"id":1009,"sortIndex":25,"affiliation":1010,"properties":24},"8a35c583-d627-4d7c-94d6-0b17a51488aa",{"id":1011,"createTime":1012,"updateTime":1012,"relativeEntities":1013,"slug":1014,"properties":1015,"entityType":53,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},"d245d185-50e3-4967-8324-acfc817042fb","2024-09-04T23:36:16.765+00:00",[],"Mekong-Institute-of-Cambodia-Phnom-Penh-Cambodia",{"title":1016},{"EN":1017},"Mekong Institute of Cambodia Phnom Penh Cambodia",{"openalex":1019,"title":1021},{"VOID":1020},"A5089196247",{"EN":1022},"Sothea 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China",{"openalex":1039,"orcid":1041,"title":1043},{"VOID":1040},"A5031092849",{"VOID":1042},"https:\u002F\u002Forcid.org\u002F0000-0001-9789-8555",{"EN":1044},"Jianshi Zhao",{"id":1046,"sortIndex":25,"researcher":24,"roles":1047,"affiliations":1048,"properties":1071},"34cb5a1d-4bb6-4a3c-b976-15f8178ef189",[],[1049,1060],{"id":1050,"sortIndex":123,"affiliation":1051,"properties":24},"60562a64-7da3-4ac8-86bd-d8f0998a0a29",{"id":1052,"createTime":1053,"updateTime":1054,"relativeEntities":1055,"slug":1056,"properties":1057,"entityType":53,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},"1794f9e5-3913-40bb-b26c-6aa905962843","2023-12-18T13:46:55.118+00:00","2024-10-15T05:11:58.057+00:00",[],"Ministry-of-Education-Key-Laboratory-for-Earth-System-Modeling-Department-of-Earth-System-Science-Tsinghua-University-Beijing-China",{"title":1058},{"VI":1059},"Ministry of Education Key Laboratory for Earth System Modeling, 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Geological observations indicate that this structure resulted from repeated stick‐slip events in the presence of highly overpressured fluids. Here we show that the major characteristics of the Glarus thrust movement (localization, periodicity, and evidence of pressurized fluids) can be reconciled by the coupling of two processes, namely, shear heating and fluid release by carbonate decomposition. During this coupling, slow ductile creep deformation raises the temperature through shear heating and ultimately activates the chemical decomposition of carbonates. The subsequent release of highly overpressurized fluids forms and lubricates the PSZ, allowing a ductile fault to move tens of kilometers on millimeter‐thick bands in episodic stick‐slip events. 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