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| ='''Chapter 11. Development of ET<sub>0</sub> computation procedure.'''= | ='''Chapter 11. Development of ET<sub>0</sub> computation procedure.'''= | ||
| - | Potential evapotranspiration (ET<sub>0</sub>) is a vital input to Water Balance calculations, which in turn are a vital part in Crop forecasting. | + | Potential evapotranspiration (ET<sub>0</sub>) is a vital input to Water Balance calculations, which in turn are a vital part in Crop forecasting. The parameters needed to calculate ET<sub>0</sub> are the following: |
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| - | The parameters needed to calculate ET<sub>0</sub> are the following: | + | |
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Revision as of 08:23, 4 August 2006
Chapter 11. Development of ET0 computation procedure.
Potential evapotranspiration (ET0) is a vital input to Water Balance calculations, which in turn are a vital part in Crop forecasting. The parameters needed to calculate ET0 are the following:
Parameter group Parameters Remarks Temperature Maximum and minimum temperature Some ET0 calculation methods use average temperature only. AgrometShell needs both minimum and maximum temperatures.
- Temperatures : minimum and maximum in degrees celcius
- Radiation. Radiation can be calculated quite accurately from the number of sunshine hours (or sunshine fraction) accompanied by Day number in the year