Multiscale Impacts of Anthropogenic and Climate Changes on Tropical and Mediterranean Hydrology
Multiscale Impacts of Anthropogenic and Climate Changes on Tropical and Mediterranean Hydrology
English[eng]
9783040000000
Africa||rainfall||monthly grids||database||inverse distance weighted||agroforestry||catchment hydrology||humid tropics||hydrological modeling||impact assessment||land-cover change||Montane Southeast Asia||rubber||trend detection||water balance||critical drought||frequency analysis||Mediterranean region||precipitation deficit||Seyhan River basin||spatial drought analysis||standardized precipitation index (SPI)||Casiquiare||Orinoco||Amazon||bifurcation||hydro-sedimentary budget||trends||Senegal River Basin||rainfall shift||hydroclimatic variables||streamflow||climate change||data preprocessing||donor selection||drainage area ratio||Euphrates basin||moving average||physical similarity||streamflow estimation||ungauged basins||water salinity||inverse estuaries||West Africa||drought||mangrove||Mono basin||extreme rainfall events||ENSEMBLE||regional climate models||modeling||MUSLE||erosion||solid transport||dam||Bouregreg||Morocco||overland flow||inter-rill erosion||teak tree plantation||understory||broom grass||South–East Asia||land management||soil erosion||flow recession model||discharge forecast||Senegal River||Gambia River||Niger River||hydroclimatology||hydrosedimentology||hydrogeochemical||Congo River Basin||urbanization||impervious area||Cameroon||runoff||Rambla de Algeciras||semi-arid||lake||lakeshores||silting||bank gullies||UAV||LiDAR||DoD||M3C2||Fouta Djallon||water tower||depletion (or recession) coefficient||runoff coefficient||soil water holding capacity||basement||sandstone||Fula society||n/a
English[eng]
9783040000000
Africa||rainfall||monthly grids||database||inverse distance weighted||agroforestry||catchment hydrology||humid tropics||hydrological modeling||impact assessment||land-cover change||Montane Southeast Asia||rubber||trend detection||water balance||critical drought||frequency analysis||Mediterranean region||precipitation deficit||Seyhan River basin||spatial drought analysis||standardized precipitation index (SPI)||Casiquiare||Orinoco||Amazon||bifurcation||hydro-sedimentary budget||trends||Senegal River Basin||rainfall shift||hydroclimatic variables||streamflow||climate change||data preprocessing||donor selection||drainage area ratio||Euphrates basin||moving average||physical similarity||streamflow estimation||ungauged basins||water salinity||inverse estuaries||West Africa||drought||mangrove||Mono basin||extreme rainfall events||ENSEMBLE||regional climate models||modeling||MUSLE||erosion||solid transport||dam||Bouregreg||Morocco||overland flow||inter-rill erosion||teak tree plantation||understory||broom grass||South–East Asia||land management||soil erosion||flow recession model||discharge forecast||Senegal River||Gambia River||Niger River||hydroclimatology||hydrosedimentology||hydrogeochemical||Congo River Basin||urbanization||impervious area||Cameroon||runoff||Rambla de Algeciras||semi-arid||lake||lakeshores||silting||bank gullies||UAV||LiDAR||DoD||M3C2||Fouta Djallon||water tower||depletion (or recession) coefficient||runoff coefficient||soil water holding capacity||basement||sandstone||Fula society||n/a