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Ocean upper pressures capture ice shelf displacement ocean surface displacement due to overlying ice shelves (see associated poster)
atmosphere->ocean fluxes are ignored (for G-compset) or diverted to the land model (for B-compset) over ice shelves
Sea ice is limited prohibited from entering ice shelf cavities
Frazil ice is limited prohibited from forming within ice shelf cavities
Runoff is routed to the ice shelf calving front instead of the ice sheet grounding line
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