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Titlebook: Estimation of Natural Groundwater Recharge; Ian Simmers (Director) Book 1988 Springer Science+Business Media Dordrecht 1988 Arid Zone.Prec

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Annette Rasmussen,Christian Ydesensivity functions. The obstacles for doing this are as follows. Taking derivatives of the spatially-distributed data, even when they are known at every point, leads to numerical instability. Hydraulic heads are always measured with inaccuracies. Differentiating this “noisy” data leads to large errors
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Cullin 3 and Its Role in Tumorigenesis,sed..It is pointed out that most models for evaporation are developed for temperate crops. The main differences between temperate and (semi-)arid regions are described..Special attention will be paid to the use of remote sensing techniques, for the determination of evaporation.
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Evaporation in Arid and Semi-Arid Regionssed..It is pointed out that most models for evaporation are developed for temperate crops. The main differences between temperate and (semi-)arid regions are described..Special attention will be paid to the use of remote sensing techniques, for the determination of evaporation.
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