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<!DOCTYPE article SYSTEM "http://www.hydrol-earth-syst-sci.net/inc/hess/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Hydrology and Earth System Sciences</journal_title>
		<journal_url>www.hydrol-earth-syst-sci.net</journal_url>
		<issn>1027-5606</issn>
		<eissn>1607-7938</eissn>
		<volume_number>1</volume_number>
		<issue_number>1</issue_number>
		<publication_year>1997</publication_year>
	</journal>
	<doi>10.5194/hess-1-93-1997</doi>
	<article_url>http://www.hydrol-earth-syst-sci.net/1/93/1997/</article_url>
	<abstract_html>http://www.hydrol-earth-syst-sci.net/1/93/1997/hess-1-93-1997.html</abstract_html>
	<fulltext_pdf>http://www.hydrol-earth-syst-sci.net/1/93/1997/hess-1-93-1997.pdf</fulltext_pdf>
	<start_page>93</start_page>
	<end_page>100</end_page>
	<publication_date>0000-00-00</publication_date>
	<article_title content_type="html">Determination of evaporation from a catchment water balance at a monthly time scale</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>H. H. G. Savenije</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">International Institute for Infrastructural, Hydraulic and Environmental Engineering (IHE), P.O. Box 3015, 2601 DA, Delft, Netherlands</affiliation>
	</affiliations>
	<abstract content_type="html">A method is presented to determine total evaporation
         from the earth&apos;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.</abstract>
	<references>
	</references>
</article>

