Multiscale Impacts of Anthropogenic and Climate Changes on Tropical and Mediterranean Hydrology

The atmospheric part of the water cycle is accelerating, affecting hydrological dynamics, especially in tropical and Mediterranean areas, where landscapes, soils and territories are particularly vulnerable to global warming and land use changes. Across four continents and a dozen of different region...

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Other Authors: Descroix, Luc (Editor), Mahé, Gil (Editor), Laraque, Alain (Editor), Ribolzi, Olivier (Editor), Lacombe, Guillaume (Editor)
Format: Electronic Book Chapter
Language:English
Published: Basel, Switzerland MDPI - Multidisciplinary Digital Publishing Institute 2021
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245 1 0 |a Multiscale Impacts of Anthropogenic and Climate Changes on Tropical and Mediterranean Hydrology 
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520 |a The atmospheric part of the water cycle is accelerating, affecting hydrological dynamics, especially in tropical and Mediterranean areas, where landscapes, soils and territories are particularly vulnerable to global warming and land use changes. Across four continents and a dozen of different regions or basins, this SI strives to highlight the environmental and societal vulnerabilities and their links with the water cycle. The basins of three of the greatest basins in the world in terms of streamflows-the Amazon River, the Orinoco River and the Congo River-show their unexpected behaviors. This book aims to present past and present status to improve future land and water management. 
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653 |a database 
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653 |a humid tropics 
653 |a hydrological modeling 
653 |a impact assessment 
653 |a land-cover change 
653 |a Montane Southeast Asia 
653 |a rubber 
653 |a trend detection 
653 |a water balance 
653 |a critical drought 
653 |a frequency analysis 
653 |a Mediterranean region 
653 |a precipitation deficit 
653 |a Seyhan River basin 
653 |a spatial drought analysis 
653 |a standardized precipitation index (SPI) 
653 |a Casiquiare 
653 |a Orinoco 
653 |a Amazon 
653 |a bifurcation 
653 |a hydro-sedimentary budget 
653 |a trends 
653 |a Senegal River Basin 
653 |a rainfall shift 
653 |a hydroclimatic variables 
653 |a streamflow 
653 |a climate change 
653 |a data preprocessing 
653 |a donor selection 
653 |a drainage area ratio 
653 |a Euphrates basin 
653 |a moving average 
653 |a physical similarity 
653 |a streamflow estimation 
653 |a ungauged basins 
653 |a water salinity 
653 |a inverse estuaries 
653 |a West Africa 
653 |a drought 
653 |a mangrove 
653 |a Mono basin 
653 |a extreme rainfall events 
653 |a ENSEMBLE 
653 |a regional climate models 
653 |a modeling 
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653 |a erosion 
653 |a solid transport 
653 |a dam 
653 |a Bouregreg 
653 |a Morocco 
653 |a overland flow 
653 |a inter-rill erosion 
653 |a teak tree plantation 
653 |a understory 
653 |a broom grass 
653 |a South-East Asia 
653 |a land management 
653 |a soil erosion 
653 |a flow recession model 
653 |a discharge forecast 
653 |a Senegal River 
653 |a Gambia River 
653 |a Niger River 
653 |a hydroclimatology 
653 |a hydrosedimentology 
653 |a hydrogeochemical 
653 |a Congo River Basin 
653 |a urbanization 
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653 |a Cameroon 
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653 |a Rambla de Algeciras 
653 |a semi-arid 
653 |a lake 
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653 |a silting 
653 |a bank gullies 
653 |a UAV 
653 |a LiDAR 
653 |a DoD 
653 |a M3C2 
653 |a Fouta Djallon 
653 |a water tower 
653 |a depletion (or recession) coefficient 
653 |a runoff coefficient 
653 |a soil water holding capacity 
653 |a basement 
653 |a sandstone 
653 |a Fula society 
653 |a n/a 
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