pastas.recharge.Peterson#
- class pastas.recharge.Peterson#
Nonlinear recharge to the groundwater.
Calculated based on Peterson and Western [2014].
The water balance for the unsaturated zone reservoir is written as:
\[\begin{split}\\frac{dS}{dt} = P_e - E_a - R\end{split}\]where the fluxes $P_e$, $E_a$ and $R$ are calculated as:
\[\begin{split}P_e = P \\left(1 - \\frac{S}{\\hat{S_{cap}}}\\right)^\\alpha\end{split}\]\[\begin{split}E_a = E_p \\left(\\frac{S}{\\hat{S_{cap}}}\\right)^\\gamma\end{split}\]\[\begin{split}R = \\hat{k_{sat}}\\left(\\frac{S}{\\hat{S_{cap}}}\\right)^{\\hat{\\beta}}\end{split}\]with the parameters:
\[\begin{split}\\hat{S_{cap}} = 10^{S_{cap}}; \\hat{k_{sat}} = 10^{k_{sat}}; \\hat{\\beta} = 10^{\\beta}\end{split}\]Note that the method currently uses forward Euler method to solve the ODE so significant water balance errors can occur.
Methods#
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Get initial parameters and bounds for the Peterson recharge model. |
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Simulate the recharge flux. |
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Calculate recharge flux sped up with numba. |
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Get the water balance for the Peterson recharge model. |