I try to set-up ROMS model for Caspian Sea. The result is little bit strange. The unrealistic cold regions over deepest regions. It seems that there is a problem in horizontal and vertical diffusion but i am not sure. I plot the surface and vertical temperature distribution and they can be seen at the end of the message. The used options are;
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/*
** Options associated with momentum equations:
*/
#define UV_ADV
#define UV_COR
#define UV_VIS2
#define UV_LDRAG
#undef UV_VIS4
/*
** Options associated with tracers equations:
*/
#define TS_U3HADVECTION
#define TS_C4VADVECTION
#define TS_DIF2
#define SALINITY
#define SOLAR_SOURCE
#undef TS_DIF4
/*
** Options for pressure gradient algorithm:
*/
#define DJ_GRADPS
#define ATM_PRESS
/*
** Options for atmospheric boundary layer:
*/
#define BULK_FLUXES
#define EMINUSP
#define LONGWAVE_OUT
/*
** Options for model configuration:
*/
#define SOLVE3D
#define MASKING
#undef STATION
/*
** Options for analytical fields configuration:
*/
#define ANA_BSFLUX
#define ANA_BTFLUX
#define ANA_INITIAL
/*
** Options for horizontal mixing of momentum:
*/
#define MIX_S_UV /* mixing along constant s surfaces */
#undef MIX_GEO_UV /* mixing on z surfaces */
#define MIX_GEO_TS
#undef MIX_S_TS
/*
** Options for vertical mixing momentum and tracers:
*/
#define MY25_MIXING
#define KANTHA_CLAYSON
#define N2S2_HORAVG
#define NONLIN_EOS
/*
** Options for close boundary conditions:
*/
#define EASTERN_WALL
#define NORTHERN_WALL
#define SOUTHERN_WALL
#define WESTERN_WALL
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Vtransform == 2 ! transformation equation
Vstretching == 2 ! stretching function
...
...
THETA_S == 8.0d0 ! surface stretching parameter
THETA_B == 0.4d0 ! bottom stretching parameter
TCLINE == 10.0d0 ! critical depth (m)
Surface temperature (Seasonal average, MAM):
1st column AVHRR
2nd column ARCLAKE
3rd column Model Results
Bathymetry and cross section positions:
Vertical cross section of temperature field (Seasonal average, MAM):
Thanks,
Regards,
--ufuk