ESTIMATION OF ACTUAL EVAPOTRANSPIRATION BY REMOTE SENSING: APPLICATION IN THESSALY PLAIN, GREECE

Tsouni, A; Koutsoyiannis, D; Kontoes, C; Mamasis, N; Elias, P

dc.contributor.author	Tsouni, A	en
dc.contributor.author	Koutsoyiannis, D	en
dc.contributor.author	Kontoes, C	en
dc.contributor.author	Mamasis, N	en
dc.contributor.author	Elias, P	en
dc.date.accessioned	2014-03-01T01:52:38Z
dc.date.available	2014-03-01T01:52:38Z
dc.date.issued	2003	en
dc.identifier.uri	https://dspace.lib.ntua.gr/xmlui/handle/123456789/26674
dc.relation.uri	http://www.itia.ntua.gr/getfile/861/1/documents/2008SensorsEvaporation.pdf	en
dc.relation.uri	http://itia.civil.ntua.gr/getfile/861/1/documents/2008sensorsevaporation.pdf	en
dc.relation.uri	http://www.itia.ntua.gr/getfile/798/1/documents/2003GISConfThessalyEvapor.pdf	en
dc.subject	Evapotranspiration	en
dc.subject	Geographic Distribution	en
dc.subject	Infrared	en
dc.subject	Remote Sensing	en
dc.subject	Satellite Data	en
dc.subject	Satellite Image	en
dc.subject	Seasonality	en
dc.subject	Surface Temperature	en
dc.subject	Wind Speed	en
dc.subject	Penman Monteith	en
dc.title	ESTIMATION OF ACTUAL EVAPOTRANSPIRATION BY REMOTE SENSING: APPLICATION IN THESSALY PLAIN, GREECE	en
heal.type	journalArticle	en
heal.publicationDate	2003	en
heal.abstract	As evapotranspiration is one of the main components of hydrologic cycle, its estimation is very important. Remote sensing technologies can assist to improve the estimation accuracy also providing means for computing evapotranspiration geographical distribution. In the present study, the daily actual evapotranspiration was calculated for 21 days uniformly distributed during the 2001 summer season over Thessaly plain. Three different methods	en