/[MITgcm]/manual/s_examples/global_oce_optim/global_oce_estimation.tex
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revision 1.6 by edhill, Wed Aug 3 15:48:06 2005 UTC revision 1.7 by molod, Tue Jun 27 19:08:22 2006 UTC
# Line 16  This experiment illustrates the optimiza Line 16  This experiment illustrates the optimiza
16  of the MITgcm. Using an ocean configuration with realistic geography and bathymetry on a  of the MITgcm. Using an ocean configuration with realistic geography and bathymetry on a
17  $4\times4^circ$ spherical polar grid, we estimate a time-independent surface heat flux correction  $4\times4^circ$ spherical polar grid, we estimate a time-independent surface heat flux correction
18  $Q_\mathrm{netm}$ that brings the model climatology into consistency with observations (Levitus  $Q_\mathrm{netm}$ that brings the model climatology into consistency with observations (Levitus
19  climatology).  climatology). The files for this experiment can be found in the verification directory under
20    tutorial\_global\_oce\_optim.
21    
22  This correction $Q_\mathrm{netm}$ (a 2D field only function of longitude and latitude) is  This correction $Q_\mathrm{netm}$ (a 2D field only function of longitude and latitude) is
23  the control variable of an optimization problem. It is inferred by an iterative  the control variable of an optimization problem. It is inferred by an iterative
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