LEADER 04058nam  2201213z- 450 
001 9910595075103321
005 20231214133242.0
035   $a(CKB)5680000000080775
035   $a(oapen)https://directory.doabooks.org/handle/20.500.12854/92084
035   $a(EXLCZ)995680000000080775
100   $a20202209d2022      |y             0
101 0 $aeng
135   $aurmn|---annan
181   $ctxt$2rdacontent
182   $cc$2rdamedia
183   $acr$2rdacarrier
200 10$aHydrological Extremes in a Warming Climate: Nonstationarity, Uncertainties and Impacts
210   $aBasel$cMDPI Books$d2022
215   $a1 electronic resource (254 p.)
311   $a3-0365-4643-X 
311   $a3-0365-4644-8 
330   $aThis 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.
517   $aHydrological Extremes in a Warming Climate
606   $aResearch & information: general$2bicssc
606   $aGeography$2bicssc
610   $aregional flood frequency analysis
610   $aflood-related attribute
610   $aregion of influence
610   $aflood region revision process
610   $aCanadian annual maximum flow
610   $aextreme precipitation
610   $aLARS-WG
610   $aCMIP5
610   $aspatiotemporal changes
610   $aclimate change
610   $aclimatic controls
610   $amultiple linear regression
610   $apermafrost region
610   $astreamflow extremes
610   $atrend analysis
610   $avariable importance analysis
610   $aextreme events
610   $ahydrology
610   $aconcurrent
610   $aColorado River basin
610   $aheatwaves
610   $adrought
610   $aflooding
610   $alow flows
610   $amulti-purpose reservoir
610   $afunctional volume
610   $auncertainties
610   $aMonte Carlo method
610   $ahydrological extremes
610   $asimulation-optimization model
610   $aoptimal storage volume
610   $asimulation model
610   $aretention volume
610   $atransformation of flood discharges
610   $aCMIP6
610   $aextreme
610   $aSWAT
610   $aflood
610   $aIHA
610   $aglobal warming
610   $aMalaysia
610   $aKelantan
610   $apeak flows
610   $apredictor
610   $apredictand
610   $asnow water equivalent
610   $aannual maximum flow
610   $awestern Canada
610   $auncertainty
610   $ariverine flooding
610   $acoastal flooding
610   $acompound flooding
610   $aprojected IDF curves
610   $adesign storm
610   $aStephenville Crossing
610   $asnow
610   $atrends
610   $aYakima River basin
610   $acascade reservoirs
610   $adesign flood
610   $anonstationary conditions
610   $aequivalent reliability
610   $amost likely regional composition
610   $adependence structure
610   $aglacier ablation
610   $aNorth Cascade Range
610   $asalmon
610   $aglacier mass balance
610   $aheat wave
615  7$aResearch & information: general
615  7$aGeography
700   $aShrestha$b Rajesh R$4edt$01332326
702   $aNajafi$b Mohammad Reza$4edt
702   $aShrestha$b Rajesh R$4oth
702   $aNajafi$b Mohammad Reza$4oth
906   $aBOOK
912   $a9910595075103321
996   $aHydrological Extremes in a Warming Climate: Nonstationarity, Uncertainties and Impacts$93040834
997   $aUNINA