Translations:Einzugsgebiet/12/en
Version vom 25. November 2020, 10:27 Uhr von Froehlich (Diskussion | Beiträge)
Evaporation has a double effect on runoff generation. On the one hand, the initial conditions in the catchment area (interception and depression storage on the surface as well as to a limited degree the soil moisture of permeable areas) are a result of the evaporation taking place before the considered precipitation event. On the other hand, the current runoff-effective precipitation is affected by the amount of the current evaporation rate. The potential (energetically possible) evaporation VP varies in time and place and is very difficult to calculate exactly. Using evaluated measurements of 20 stations, the mean values of which are presented in the following histogram, the following compensation function was determined /BRANDT, 1979/.