Determination of evaporation from a catchment water balance at a monthly time scale

A method is presented to determine total evaporation from the earth's surface at a spatial scale that is adequate for linkage with climate models. The method is based on the water balance of catchments, combined with a calibrated autoregressive rainfall-runoff model. The time scale used is...

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Main Author: H. H. G. Savenije
Format: Article
Language:English
Published: Copernicus Publications 1997-01-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/1/93/1997/hess-1-93-1997.pdf
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author H. H. G. Savenije
author_facet H. H. G. Savenije
author_sort H. H. G. Savenije
collection DOAJ
description A method is presented to determine total evaporation from the earth's surface at a spatial scale that is adequate for linkage with climate models. The method is based on the water balance of catchments, combined with a calibrated autoregressive rainfall-runoff model. The time scale used is in the order of decades (10 days) to months. The rainfall-runoff model makes a distinction between immediate processes (interception and short term storage) and the remaining longer-term processes. Besides the calibrated rainfall-runoff model and the time series of observed rainfall and runoff, the method requires a relation between transpiration and soil moisture storage. The method is applied to data of the Bani catchment in Mali, a sub-catchment of the Niger river basin.
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spelling doaj.art-81a1500ed99b4abca9123aa699a93b522022-12-22T02:51:43ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79381997-01-011193100Determination of evaporation from a catchment water balance at a monthly time scaleH. H. G. SavenijeA method is presented to determine total evaporation from the earth's surface at a spatial scale that is adequate for linkage with climate models. The method is based on the water balance of catchments, combined with a calibrated autoregressive rainfall-runoff model. The time scale used is in the order of decades (10 days) to months. The rainfall-runoff model makes a distinction between immediate processes (interception and short term storage) and the remaining longer-term processes. Besides the calibrated rainfall-runoff model and the time series of observed rainfall and runoff, the method requires a relation between transpiration and soil moisture storage. The method is applied to data of the Bani catchment in Mali, a sub-catchment of the Niger river basin.http://www.hydrol-earth-syst-sci.net/1/93/1997/hess-1-93-1997.pdf
spellingShingle H. H. G. Savenije
Determination of evaporation from a catchment water balance at a monthly time scale
Hydrology and Earth System Sciences
title Determination of evaporation from a catchment water balance at a monthly time scale
title_full Determination of evaporation from a catchment water balance at a monthly time scale
title_fullStr Determination of evaporation from a catchment water balance at a monthly time scale
title_full_unstemmed Determination of evaporation from a catchment water balance at a monthly time scale
title_short Determination of evaporation from a catchment water balance at a monthly time scale
title_sort determination of evaporation from a catchment water balance at a monthly time scale
url http://www.hydrol-earth-syst-sci.net/1/93/1997/hess-1-93-1997.pdf
work_keys_str_mv AT hhgsavenije determinationofevaporationfromacatchmentwaterbalanceatamonthlytimescale