Difference between revisions of "Geostrophic Initialization"
From MohidWiki
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SUBMODEL : 0 | SUBMODEL : 0 | ||
MISSING_NULL : 1 | MISSING_NULL : 1 | ||
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WIND : 1 | WIND : 1 | ||
ATM_PRESSURE : 1 | ATM_PRESSURE : 1 |
Revision as of 10:47, 31 January 2012
Description
In this initialization methodology all forces are switched (except tidal force) at the first iteration. The velocity and sea surface height initial fields have non zero values consistent with the salinity and temperature initial fields, trough the geostrophic equilibrium. If the initialization is made in a level 2 embedded in a 2D tidal model (level 1), tidal force must be switched progressively along a selected period (in level 1).
Example File
Hydrodynamic_1.dat OUTPUT_TIME : 0 3600 SURFACE_OUTPUT_TIME : 0 3600 GEOST_INITIALIZATION : 1 ! Select geostrophic initialization SUBMODEL_FATHER_HOT_START : 0 ! must be zero for embedded models to prevent the imposition of father values ! Water level initial solution imposed <begin_waterlevel> NAME : water level DEFAULTVALUE : 0 INITIALIZATION_METHOD : HDF FILENAME : ..\..\GeneralData\Mercator\Mercator_ANA_Level2_Jun.hdf5 TYPE_ZUV : z ADDING_FACTOR : 0.0 ! This factor adds to the mean level of the Initial Solution <end_waterlevel> TIDE : 0 TIDEPOTENTIAL : 1 ! If model run embedded in a 2D tide model CONTINUOUS : 0 ! The model cannot be a continous run DATA_ASSIMILATION : 1 BRFORCE : 1 BRGEOMETRY : 1 BRWATERLEVEL : 0 RADIATION : 2 LOCAL_SOLUTION : 3 SUBMODEL : 0 MISSING_NULL : 1 WIND : 1 ATM_PRESSURE : 1 ATM_PRESSURE_TYPE : 2 ATM_RAMP : 0 ATM_PERIOD : 86400 IMPOSE_INVERTED_BAROMETER : 1 BIHARMONIC : 1 BIHARMONIC_COEF : 1e10