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Hydrol. Earth Syst. Sci., 1, 93-100, 1997
www.hydrol-earth-syst-sci.net/1/93/1997/
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Determination of evaporation from a catchment water balance at a monthly time scale

H. H. G. Savenije
International Institute for Infrastructural, Hydraulic and Environmental Engineering (IHE), P.O. Box 3015, 2601 DA, Delft, Netherlands

Abstract. 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.

Final Revised Paper (PDF, 3474 KB)

Citation: Savenije, H. H. G.: Determination of evaporation from a catchment water balance at a monthly time scale, Hydrol. Earth Syst. Sci., 1, 93-100, 1997.   Bibtex   EndNote   Reference Manager