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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