Abstract
(1) Evapotranspiration from a marshy meadow in southern Bohemia, Czechoslovakia, was determined over the period April to November 1977, by measuring water losses from a tank installed within the area and planted with the local vegetation. (2) Simultaneously, heat balance components were calculated by the Bowenratio method from climatic data recorded at hourly intervals on each day during the measurement period. (3) The daily, weekly and monthly course of the heat-balance components and their totals are given. (4) 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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