00871cam0 2200253 450 E60020003223820200331083513.020071211d1990 |||||ita|0103 baitaIT<<Il >>Museo Anatomicocur. Antonio CastroNapoliArte Tipografica199020 p.104 ill25 cmCastro, AntonioA600200045279070*Università degli studi di Napoli Federico II, Facoltà di Medicina VeterinariaA600200045278070333373ITUNISOB20200331RICAUNISOBUNISOB50090101E600200032238M 102 Monografia moderna SBNM500000444SI90101donopregresso2UNISOBUNISOB20071211080728.020200330073250.0SpinosaMuseo Anatomico1687798UNISOB04094nam 2201237z- 450 991059507510332120230220(CKB)5680000000080775(oapen)https://directory.doabooks.org/handle/20.500.12854/92084(oapen)doab97406(EXLCZ)99568000000008077520202209d2022 |y 0engurmn|---annantxtrdacontentcrdamediacrrdacarrierHydrological Extremes in a Warming ClimateNonstationarity, Uncertainties and ImpactsBaselMDPI - Multidisciplinary Digital Publishing Institute20221 online resource (254 p.)3-0365-4643-X 3-0365-4644-8 This Special Issue comprises 11 papers that outline the advances in research on various aspects of climate change impacts on hydrologic extremes, including both drivers (temperature, precipitation, and snow) and effects (peak flow, low flow, and water temperature). These studies cover a broad range of topics on hydrological extremes, including hydro-climatic controls, trends, homogeneity, nonstationarity, compound events and associated uncertainties, for both historical and future climates.Hydrological Extremes in a Warming ClimateGeographybicsscResearch & information: generalbicsscannual maximum flowCanadian annual maximum flowcascade reservoirsclimate changeclimatic controlsCMIP5CMIP6coastal floodingColorado River basincompound floodingconcurrentdependence structuredesign flooddesign stormdroughtequivalent reliabilityextremeextreme eventsextreme precipitationfloodflood region revision processflood-related attributefloodingfunctional volumeglacier ablationglacier mass balanceglobal warmingheat waveheatwaveshydrological extremeshydrologyIHAKelantanLARS-WGlow flowsMalaysiaMonte Carlo methodmost likely regional compositionmulti-purpose reservoirmultiple linear regressionn/anonstationary conditionsNorth Cascade Rangeoptimal storage volumepeak flowspermafrost regionpredictandpredictorprojected IDF curvesregion of influenceregional flood frequency analysisretention volumeriverine floodingsalmonsimulation modelsimulation-optimization modelsnowsnow water equivalentspatiotemporal changesStephenville Crossingstreamflow extremesSWATtransformation of flood dischargestrend analysistrendsuncertaintiesuncertaintyvariable importance analysiswestern CanadaYakima River basinGeographyResearch & information: generalShrestha Rajesh Redt1332326Najafi Mohammad RezaedtShrestha Rajesh RothNajafi Mohammad RezaothBOOK9910595075103321Hydrological Extremes in a Warming Climate4425578UNINA