Berendrecht¶
- class Berendrecht[source]¶
Recharge to the groundwater calculated according to [berendrecht_2006].
Notes
Note that the preferred unit of the precipitation and evaporation is mm/d. The waterbalance for the unsaturated zone reservoir is written as:
\[\frac{dS_e}{dt} = \frac{1}{D_e}(f_iP - E_a - R)\]where the recharge is calculated as:
\[R(S_e) = K_sS_e^\lambda(1-(1-S_e^{1/m})^m)^2\]For a detailed description of the recharge model and parameters we refer to the original publication.
References
- berendrecht_2006
Berendrecht, W. L., Heemink, A. W., van Geer, F. C., and Gehrels, J. C. (2006) A non-linear state space approach to model groundwater fluctuations, Advances in Water Resources, 29, 959–973.
Methods¶
Initialize self. |
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Method to obtain the initial parameters. |
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Internal method used for the recharge calculation. |
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Simulate the recharge flux. |