For the old hydrology scheme (itype_hydmod = 0) the calculation of the subsurface runoff has been improved, in order to better close the soil water budget.
For itype_hydmod = 1 a zero-flux condition is applied at the lower boundary of the hydrological active layers. No fix is required for that.
The changes have no impact on any prognostic variable.
The debug output has been modified to check the soil water budget at a specific grid point (first meteograph point).
Introduced a new field res_soilwatb for the soil water budget (residuum).
shortname | COSMO variable | Explanation | Unit |
---|---|---|---|
RESID_WSO | res_soilwatb | soil water budget, residuum | kg/m2 |
This field can be interpreted as an aggregation of all hydrological active soil layers. Therefore it is coded in GRIB as a "depthBelowLandLayer" with upper level 0 and lower level ibot_w_so (number of hydrological active soil layers; in TERRA called ke_soil_hy).
A logical switch in data_runcontrol (lres_soilwatb) is set to .TRUE., if RESID_WSO appears in an output list. Only then the necessary computations are done in sfc_terra.f90.
There are problems with these variables (wt_depth, wso_satlev, q_roff, wsoil_flx): (Modifications in sfc_terra.f90, sfc_interface.f90, src_output.f90)
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