An advection-aridity approach to estimate actual regional evapotranspiration

Brutsaert, W; Stricker, H

dc.contributor.author	Brutsaert, W	en
dc.contributor.author	Stricker, H	en
dc.date.accessioned	2014-03-01T01:05:44Z
dc.date.available	2014-03-01T01:05:44Z
dc.date.issued	1979	en
dc.identifier.uri	https://dspace.lib.ntua.gr/xmlui/handle/123456789/8951
dc.subject	Evapotranspiration	en
dc.title	An advection-aridity approach to estimate actual regional evapotranspiration	en
heal.type	journalArticle	en
heal.identifier.primary	10.1029/WR015i002p00443	en
heal.identifier.secondary	http://dx.doi.org/10.1029/WR015i002p00443	en
heal.publicationDate	1979	en
heal.abstract	Actual regional evapotranspiration is calculated by means of a procedure requiring only meteorological data, which are those commonly used in the various versions of the combination approach for potential evaporation. The approach is based on a conceptual model involving, first, the effect of regional advection on potential evaporation, and second, an assumed symmetry between potential and actual evaporation with respect	en
heal.journalName	Water Resources Research	en
dc.identifier.doi	10.1029/WR015i002p00443	en