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- W1970910879 abstract "[1] Processes at the ice shelf-ocean interface and in particular in ice shelf cavities around Antarctica have an observable effect on the solutions of basin scale to global coupled ice-ocean models. Despite this, these processes are not routinely represented in global ocean and climate models. It is shown that a new ice shelf cavity model for z coordinate models can reproduce results from an intercomparison project of earlier approaches with vertical σ or isopycnic coordinates. As a proof of concept, ice shelves are incorporated in a 100-year global integration of a z coordinate model. In this simulation, glacial meltwater can be traced as far as north as 15°S. The observed effects of processes in the ice shelf cavities agree with previous results from a σ coordinate model, notably the increase in sea ice thickness. However, melt rates are overestimated probably because the parameterization of basal melting does not suit the low resolution of this configuration." @default.
- W1970910879 created "2016-06-24" @default.
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- W1970910879 date "2008-08-26" @default.
- W1970910879 modified "2023-10-14" @default.
- W1970910879 title "Modeling ice shelf cavities in a<i>z</i>coordinate ocean general circulation model" @default.
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- W1970910879 doi "https://doi.org/10.1029/2007jc004368" @default.
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