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HadCM3
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== Coupling == The atmospheric model is run for a day, and the fluxes (of heat, moisture and momentum) at the atmosphere-ocean interface are accumulated. Then the ocean model is run for a day, with the reverse fluxes accumulated. This then repeats through the length of the run. Unlike its predecessor HadCM2 there is no need for ''flux correction''βthe model climate remains stable and does not significantly drift. The lack of flux correction is cited by the IPCC as one of the advances in modelling since the [[IPCC Second Assessment Report]].<ref>{{cite web|url=http://www.grida.no/climate/ipcc_tar/wg1/309.htm|title=Climate Change 2001: The Scientific Basis|work=grida.no|url-status=dead|archive-url=https://web.archive.org/web/20050305043239/http://www.grida.no/climate/ipcc_tar/wg1/309.htm|archive-date=5 March 2005}}</ref> The ocean model incorporates a thermodynamic-dynamic sea ice model with primitive (ocean drift) dynamics.
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