The Improvement of the Lake Most Evaporation Estimates

Abstract

The Lake Most represents extensive hydric reclamation of the former surface mine of Most–Ležáky, which is unique in the sense that it does not have a natural inflow and runoff. The main goal of the ongoing research is to costruct a mathematical model predicting the water balance of Lake Most. Therefore, it is important to separate amount of water that is lost by the evaporation and amount of water that is lost into the subsoil. In this article, we focus on the possibilities of evaporation estimates and their improvements.