/[MITgcm]/MITgcm/verification/lab_sea/README
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revision 1.1.2.8 by dimitri, Tue Mar 11 21:26:04 2003 UTC revision 1.1.2.9 by dimitri, Wed Apr 30 04:55:13 2003 UTC
# Line 202  results from exp3a and exp3b: Line 202  results from exp3a and exp3b:
202    lookat_exp3    lookat_exp3
203    
204  If the dynamic ice solvers are correct, they should converge to a  If the dynamic ice solvers are correct, they should converge to a
205  constant solution.  The tests above show that both the ADI and the LSR  solution that is constant at each latitude.
 solver are unable to handle periodic domains and therefore that they  
 cannot be "correctly" parallelized.  
206    
207    
208  Instructions for running Experiment 4  Instructions for running Experiment 4
# Line 232  NPSEUDO in data.seaice at the expense of Line 230  NPSEUDO in data.seaice at the expense of
230  Also as sea-ice ages (thickens) the difference at the tiles becomes  Also as sea-ice ages (thickens) the difference at the tiles becomes
231  increasingly small.  For solver pkg/seaice/adi.F a value of NPSEUDO=10  increasingly small.  For solver pkg/seaice/adi.F a value of NPSEUDO=10
232  appears adequate for forward integrations but cannot be used for sea-ice  appears adequate for forward integrations but cannot be used for sea-ice
233  adjoint model.  Work is underway to fix this problem.  adjoint model.  With NPSEUDO=300 or greater, the tile disappears, but the
234    computational cost is very large (11 times that of teh forward model).
235    
236    
237  Instructions for running Experiment 5  Instructions for running Experiment 5
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