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R. J. Murray, Nathaniel L. Bindoff, and C. J. C. Reason

drift is negligible in comparison with the interannual changes of 0.2°–1°C, which occurred in waters down to 1500 m during the transient simulations. The model ocean was global except for the Arctic seas, which were considered unimportant for this study and were blocked at the Greenland–Iceland–Scotland Ridge. No sea ice model was used, as the water properties in the (mainly Southern Hemisphere) sea ice regions were forced by prescribed and restoration fluxes in the same way as in open ocean regions

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