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  4. International Symposium on Hydrology of Mountainous Areas, 28-30 May 1992 at Shimla (India).
Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/3554
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dc.contributor.authorMiklanek, P.-
dc.date.accessioned2019-09-12T12:10:13Z-
dc.date.available2019-09-12T12:10:13Z-
dc.date.issued1992-
dc.identifier.urihttp://117.252.14.250:8080/jspui/handle/123456789/3554-
dc.description.abstractEvapotranspiration 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.isoenen_US
dc.publisherNational Institute of Hydrologyen_US
dc.subjectEvapotranspirationen_US
dc.subjectTatra mountains in Central Europeen_US
dc.title1.2-Evapotranspiration in the Tatra mountains in Central Europeen_US
dc.typeTechnical Reporten_US
Appears in Collections:International Symposium on Hydrology of Mountainous Areas, 28-30 May 1992 at Shimla (India).

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