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ISHS Acta Horticulturae 278: Symposium on Scheduling of Irrigation for Vegetable Crops under Field Condition

EVALUATION OF EVAPOTRANSPIRATION BY COMBINING PLANT CHARACTERISTICS AND METEOROLOGICAL INFORMATION

Authors:   M. Meron, M. Fuchs, I. Levin, R. Halel, R. Feuer
Abstract:
Three methods of Evapo-Transpiration measurements were tested at the Field Crops Experimental Farm of the Upper Galilee Regional Council at the Hula Valley of Israel, in 1987:
  • A modified Penman (1948) equation, summed diurnal or daylight time only;
  • The same Penman equation, but the radiation term factored with canopy light interception;
  • A modified Monteith (1965) type equation (Fuchs et al., 1987).

Radiation, windspeed, air temperature and relative humidity (RH) were measured with an automatic weather station at 2.0 m above ground. A USWB Class "A" evaporation pan was located nearby.

Plant data were collected at a cotton field (cv. SJ-2), drip irrigated daily with 3 water amounts at 2 timings, creating 6 different canopy shapes and stress levels.

Soil water balance, calculated from weekly neutron probe measurements, was used to estimate actual ET.

Diurnal Penman ET was about 96.5 % of Pan ET. When summed over daylight hours only, it comprised 85.6% of Pan ET, similar to the crop coefficient recommended for drip irrigated cotton.

Two models were used: LI (light interception) factored Penman ET, and the Fuchs model described 91.5 % of soil water balance ET when summed over full season. There was a considerable variation in matching the monthly data that was measured and modeled. For practical irrigation scheduling purposes, however, both models look equally adequate.

A pilot regional irrigation scheduling information service, using LI corrected Penman model, was started in 1988 and was turned permanent this year, after positive evaluation.

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