Climate variability and change in the 21th Century
- 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...
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Format | eBook |
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Language | English |
Published |
Basel, Switzerland
MDPI - Multidisciplinary Digital Publishing Institute
2021
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Subjects | |
Online Access | Get full text |
ISBN | 3036501096 9783036501093 3036501088 9783036501086 |
DOI | 10.3390/books978-3-0365-0109-3 |
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Abstract | - 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. |
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AbstractList | - 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. |
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SubjectTerms | acclimatization Aqua Bayesian-model averaging bias correction bias correction methods boreal region California Caucasian region climate climate change climate change and Conakry climate classification climate indices climate manipulation climate model selection climate-fire models cluster analysis CMIP5 CO2 fertilization effect CORDEX Côte d’Ivoire downscaling drought droughts ENSO ERA5 excess heat factor extreme wind speed feedback GCM geoengineering Google Earth Engine GPP Greece heat wave Hluhluwe-iMfolozi Park Hurst exponent hydrologic regions hydrological modeling intercalibration intersensor comparison kriging interpolation LAI Mann–Kendall Mediterranean climate mega-fires model uncertainty MODIS Mono River watershed multiple climate models multivariate NDVI objective classification OLCI optimal control persistence precipitation precipitations pseudo reality rainfall RCM Reference, Information and Interdisciplinary subjects reflective solar bands Regional Climate Model regional climate modeling Research and information: general RSB sassandra watershed Sentinel-3A SNO SNPP soil frost spatial correlation standardized precipitation index (SPI) surface roughness temperature Terra terrestrial ecosystems time series analysis topography trend analysis upper Indus basin VIIRS Vu Gia-Thu Bon warming wavelet weights wind climate wind damage risk management wind multiplier |
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Title | Climate variability and change in the 21th Century |
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