A copy of this work was available on the public web and has been preserved in the Wayback Machine. The capture dates from 2018; you can also visit the original URL.
The file type is
AbstractAi r temperature, sunshine duration and precipitation are used to estimate the soil moisture in the shallow root zone. The model for the estimation of the soil moisture is based on the water balance of the root zone. The daily amount of evapotranspiration was estimated using the Priestley and Taylor model, modified by the ratio of total soil moisture and soil moisture at the field capacity in a given soil layer. The upward capillary flow was evaluated from the unsaturated hydraulicdoi:10.2480/agrmet.48.851 fatcat:xrjcsakasjb5tiwafcbzbrwpkq