[MITgcm-devel] description of seaice parameters
Dimitris Menemenlis
menemenlis at sbcglobal.net
Tue Sep 13 23:23:56 EDT 2005
Hi Martin, thanks for sweeping through pkg/seaice. That's really
helpful. A few more comments in addition to Jinlun's:
> The biggest difference is in SEAICE_freeze, which is -1.96degC in
> seaice_readparms.F, but -1.86degC in his code. Maybe still another
> reason for the thin ice around Antarctica and the large erroneous
> polynyas in the high-res cubed sphere experiments.
I have run a sensitivity experiment with -1.8 deg C freezing point,
which gives slightly thicker ice around Antarctica, as expected.
Eventually, I assume we will want this to depend on salinity.
> Also he uses a smaller value of pstart=1.5e4 (instead of
> SEAICE_strength=2.75e4 in seaice_readparms.F). Only FYI.
I have also run a sensitivity experiment for this parameter. Slightly
larger, rather than lower, pstar seems to help reduce the Polynya problem.
> However, we found that the parameters
> SEAICE_sensHeat/latentWater/latentIce are not really the coefficients
> as described in SEAICE_READPARMS.h but (density of air)*(heat
> capacity of air/latent heat of water/latent heat of ice)*(transfer
> coefficient)
> At least, that's what we found by comparing the code and default
> values. If you want me to do it I'll change the description in
> SEAICE_READPARAMS.h to reflect this, so that future seaice-novices do
> not stumble over this?
I remember working out what these constants actually were at some point
in time and that there were some scaling factors. But I forgot to add
the scaling factors to descriptions in SEAICE_PARAMS.h as I should have.
It would be great if you can update the definitions.
Dimitris
--
Dimitris Menemenlis <menemenlis at jpl.nasa.gov>
Jet Propulsion Lab, California Institute of Technology
MS 300-323, 4800 Oak Grove Dr, Pasadena CA 91109-8099
tel: 818-354-1656; fax: 818-393-6720
More information about the MITgcm-devel
mailing list