[MITgcm-support] interpolate sea ice fields
Daiwei (David) Wang
daiwei at MIT.EDU
Thu Aug 18 10:51:39 EDT 2011
Hi Martin,
Thanks for the comment.
Computationally sub-sampling should be OK. But I hope the interpolated
fields best approximate the original fields. For example, since one new
grid cell comprises 25 old grid cells, for siAREA,
siAREA_new = sum(siAREA_old*RAC)/sum(RAC)
would conserve total sea ice concentration (where RAC is the cell area
of the old grid), and presumably be a better choice than sub-sampling.
But I'm not sure about other sea ice fields.
Thanks,
David
On 8/18/11 4:10 AM, Martin Losch wrote:
> Hi David,
>
> the model should be able to deal with subsampled sea-ice fields (i.e. not blow up), if that's the question.
>
> Martin
>
> On Aug 17, 2011, at 8:01 PM, Daiwei (David) Wang wrote:
>
>> Hi,
>>
>> I intend to interpolate a set of pickup files to a grid five times (horizontally) coarser than the original grid, and wonder what the most appropriate means of interpolation is for sea ice fields, which are
>>
>> $ cat pickup_seaice.0000000001.meta
>> nDims = [ 2 ];
>> dimList = [
>> 3060, 1, 3060,
>> 510, 1, 510
>> ];
>> dataprec = [ 'float64' ];
>> nrecords = [ 13 ];
>> timeStepNumber = [ 26280 ];
>> /* modelTime = [ 3.153600000000E+07 ];*/
>> nFlds = [ 7 ];
>> fldList = {
>> 'siTICES ' 'siAREA ' 'siHEFF ' 'siHSNOW ' 'siHSALT ' 'siUICE ' 'siVICE'
>> };
>>
>> Will naive sub-sampling of every five grid points do, or area-weighted averaging?
>>
>> Thanks,
>> David
>>
>>
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>> MITgcm-support at mitgcm.org
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>
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--
Daiwei Wang, Postdoctoral Associate
54-1517, Program in Atmospheres, Oceans, and Climate
Department of Earth, Atmospheric and Planetary Sciences
Massachusetts Institute of Technology
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