1.2-Evapotranspiration in the Tatra mountains in Central Europe

dc.contributor.author	Miklanek, P.
dc.date.accessioned	2019-09-12T12:10:13Z
dc.date.available	2019-09-12T12:10:13Z
dc.date.issued	1992
dc.identifier.uri	http://117.252.14.250:8080/jspui/handle/123456789/3554
dc.description.abstract	Evapotranspiration in the mountains represents an important water balance element. Unfortunately, our knowledge and possibilities for its direct determination are only limited. Results of the actual evapotranspiration Mountains are presented. complex method. Totally 10 115 m a.s.l . to 2635 m a.s.l analysis of both potential and in Central European Tatra The calculations are based on stations in elevation range from in 1956-1980 period were used. The role of evapotranspiration in the water balance is described by means of comparison with precipitation amounts.	en_US
dc.language.iso	en	en_US
dc.publisher	National Institute of Hydrology	en_US
dc.subject	Evapotranspiration	en_US
dc.subject	Tatra mountains in Central Europe	en_US
dc.title	1.2-Evapotranspiration in the Tatra mountains in Central Europe	en_US
dc.type	Technical Report	en_US