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enhancementNew feature or requestNew feature or request
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The numerical solution for wave attenuation in sea ice employs time splitting, which is only order dtg accurate. It is a noticeable error when dtg > 500 s or so. I've included a pdf to illustrate the error.
I recommend two solutions. (1) first don't use time splitting for the sea ice attenuation and instead include the sea ice "source" with the other sources and (2) employ subcycling on the global time step when the sea ice concentration is between say 5 and 95%. Happy to provide code.
Reducing dtg is a costly alternative.
See attached pdf
TimeSplittingProblem.pdf
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enhancementNew feature or requestNew feature or request