class-u3m-1d -- CLASS Unsaturated Moisture Movement Model U3M-1D

 

About class-u3m-1d

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CLASS Unsaturated Moisture Movement Model U3M-1D can be used for partitioning water balance using Richards' equation in the unsaturated zone for any combination of climate conditions, land-use and soil type. Non-reactive solute balance across the soil profile can also be performed using advective transport. A balance is conducted for each soil material and evaporative, drainage and solute fluxes are simulated over time. Water balance error associated with the numerical approximation is quantified for each soil material. The model uses an adaptable sub-daily time step based on transient climate conditions.

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