05047nam 2201405z- 450 991055754760332120231214132820.0(CKB)5400000000044130(oapen)https://directory.doabooks.org/handle/20.500.12854/68309(EXLCZ)99540000000004413020202105d2021 |y 0engurmn|---annantxtrdacontentcrdamediacrrdacarrierClimate variability and change in the 21th CenturyBasel, SwitzerlandMDPI - Multidisciplinary Digital Publishing Institute20211 electronic 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: generalbicsscCaliforniahydrologic regionswarmingdroughtregional climate modelinghydrological modelingbias correctionmultivariatepseudo realityrainfalltrend analysisMann–Kendallkriging interpolationmultiple climate modelsstandardized precipitation index (SPI)droughtsweightsVu Gia-Thu Bonclimate changeoptimal controlgeoengineeringclimate manipulationGCMRCMCMIP5CORDEXclimate model selectionupper Indus basinNDVIENSOwavelettime series analysisHluhluwe-iMfolozi ParkGoogle Earth EngineMediterranean climatecluster analysisobjective classificationERA5mega-firesBayesian-model averagingmodel uncertaintyclimate-fire modelsMono River watershedclimatetemperatureheat waveexcess heat factoracclimatizationGreeceprecipitationsHurst exponentpersistencespatial correlationCaucasian regionRegional Climate Modelclimate classificationbias correction methodsprecipitationterrestrial ecosystemsGPPLAICO2 fertilization effectfeedbacksassandra watershedCôte d’Ivoireboreal regionextreme wind speedwind climatesoil frostwind damage risk managementwind multiplierdownscalingtopographysurface roughnessVIIRSMODISOLCIRSBSNPPTerraAquaSentinel-3Areflective solar bandsintersensor comparisonintercalibrationSNOclimate indicesclimate change and ConakryResearch & information: generalStefanidis Stefanosedt1302986Tolika KonstantiaedtStefanidis StefanosothTolika KonstantiaothBOOK9910557547603321Climate variability and change in the 21th Century3026808UNINA