05059nam 2201417z- 450 991055754760332120210501(CKB)5400000000044130(oapen)https://directory.doabooks.org/handle/20.500.12854/68309(oapen)doab68309(EXLCZ)99540000000004413020202105d2021 |y 0engurmn|---annantxtrdacontentcrdamediacrrdacarrierClimate variability and change in the 21th CenturyBasel, SwitzerlandMDPI - Multidisciplinary Digital Publishing Institute20211 online resource (384 p.)3-0365-0108-8 3-0365-0109-6 - Water resources management should be assessed under climate change conditions, as historic data cannot replicate future climatic conditions. - Climate change impacts on water resources are bound to affect all water uses, i.e., irrigated agriculture, domestic and industrial water supply, hydropower generation, and environmental flow (of streams and rivers) and water level (of lakes). - Bottom-up approaches, i.e., the forcing of hydrologic simulation models with climate change models' outputs, are the most common engineering practices and considered as climate-resilient water management approaches. - Hydrologic simulations forced by climate change scenarios derived from regional climate models (RCMs) can provide accurate assessments of the future water regime at basin scales. - Irrigated agriculture requires special attention as it is the principal water consumer and alterations of both precipitation and temperature patterns will directly affect agriculture yields and incomes. - Integrated water resources management (IWRM) requires multidisciplinary and interdisciplinary approaches, with climate change to be an emerging cornerstone in the IWRM concept.Research & information: generalbicsscacclimatizationAquaBayesian-model averagingbias correctionbias correction methodsboreal regionCaliforniaCaucasian regionclimateclimate changeclimate change and Conakryclimate classificationclimate indicesclimate manipulationclimate model selectionclimate-fire modelscluster analysisCMIP5CO2 fertilization effectCORDEXCôte d'IvoiredownscalingdroughtdroughtsENSOERA5excess heat factorextreme wind speedfeedbackGCMgeoengineeringGoogle Earth EngineGPPGreeceheat waveHluhluwe-iMfolozi ParkHurst exponenthydrologic regionshydrological modelingintercalibrationintersensor comparisonkriging interpolationLAIMann-KendallMediterranean climatemega-firesmodel uncertaintyMODISMono River watershedmultiple climate modelsmultivariateNDVIobjective classificationOLCIoptimal controlpersistenceprecipitationprecipitationspseudo realityrainfallRCMreflective solar bandsRegional Climate Modelregional climate modelingRSBsassandra watershedSentinel-3ASNOSNPPsoil frostspatial correlationstandardized precipitation index (SPI)surface roughnesstemperatureTerraterrestrial ecosystemstime series analysistopographytrend analysisupper Indus basinVIIRSVu Gia-Thu Bonwarmingwaveletweightswind climatewind damage risk managementwind multiplierResearch & information: generalStefanidis Stefanosedt1302986Tolika KonstantiaedtStefanidis StefanosothTolika KonstantiaothBOOK9910557547603321Climate variability and change in the 21th Century3026808UNINA