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.
