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SVERIGES LANTBRUKSUNIVERSITET - Epsilon Open Archive - SLU

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92<br />

Brief deseription of the eomputer programs developed is<br />

given exeluding all mathematieal equations. The main em­<br />

phasis is devoted to the input variables needed in the models<br />

and to the output variables eomputed by the simulation<br />

programs.<br />

Program 1: CropWP - eomputation of erop water balanee and<br />

eanopy photosynthesis on a seasonal basis<br />

The purpose of this program is to eompute the water<br />

balanee of the eropincluding estimation of transpiration and<br />

crop photosynthesis over the whole growing season. The<br />

effect of soil water content on transpiration and erop photo­<br />

synthesis is taken into aceount. This program can be used to<br />

predict the need for irrigation when soil type and the meteo­<br />

rological driving variables are known. Soil parameters can<br />

be taken based on so il texture as described by Driessen<br />

(1986) or pF-curve and hydraulic conduetivity funetion can<br />

be measured directly.<br />

The meteorological input variables needed are:<br />

· solar radiation<br />

· air temperature<br />

• precipitation<br />

• relative humidity or vapour pressure deficit (VPD)<br />

· wind speed<br />

The most important parameters needed are:<br />

• crop biomass allocation over various plant organs<br />

• crop light response curve (photosynthetically active<br />

radiation versus leaf photosynthesis)<br />

• soil pF-curve and hydraulic conductivity<br />

The program CropWP is capable of eomputing potential and<br />

actual transpiration and photosynthesis rates on a daily<br />

basis. Moreover, the soil water content profile can be<br />

computed.<br />

The computation of crop water balance is largely based<br />

on ideas presented by Federer (1979) and Choudhury and Idso<br />

(1985a and 1985b). The computation of canopy photosynthesis<br />

resembles very closely the methods presented by Spitters<br />

(1986) and Spitters et al. (1986). The models for computa­<br />

tion of soil water balance have been described by Karvonen<br />

(1988). Unfortunately there exist so far no complete data

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