Abstract
Evapotranspiration from a marshy meadow in southern Bohemia, Czechoslovakia, was determined over the period April-Nov. 1977, by measuring water losses from a tank installed within the area and planted with the local vegetation. Simultaneously, heat balance components were calculated by the Bowen-ratio method from climatic data recorded at hourly intervals on each day during the measurement period. The daily, weekly and monthly course of the heat-balance components and their totals are given. Mean daily evapotranspiration during the period of measurement was 2.6 mm, and the maximum daily value in summer was 6.5 mm.

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