/[MITgcm]/MITgcm/verification/ideal_2D_oce/README
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revision 1.1 by jmc, Fri Jan 17 14:17:58 2003 UTC revision 1.2 by jmc, Mon Mar 10 01:35:16 2014 UTC
# Line 1  Line 1 
1  test - experiment : ideal_2D_oce  test - experiment : ideal_2D_oce
2    
3  purpose: Shows that the residual mean circulation is becoming small  purpose: Shows that the residual mean circulation is becoming small
4   at the Equilibrium (Bolus cancel the Euleurian circ.) and is function   at the Equilibrium (Bolus cancel the Euleurian circ.) and is function
5   of the diapycnal mixing.   of the diapycnal mixing.
6    
7  Set up:  Set up:
8   Idealized 2D global ocean with flat bathymetry and no continent,   Idealized 2D global ocean with flat bathymetry and no continent,
9   symetric relative to the Eq.   symetric relative to the Eq.
10   Forcing: zonal wind stress and surface temp. relaxation toward a   Forcing: zonal wind stress and surface temp. relaxation toward a
11   "realistic" SST (function of Latitude).   "realistic" SST (function of Latitude).
12    
13  To reduce diapycnal mixing, "exotic" parameters are used (and tested)  To reduce diapycnal mixing, "exotic" parameters are used (and tested)
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