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- W134202456 abstract "The results presented here allow us to argue that the similarity of the CMIP3-simulated SST response to the observed one (Fig. 1), despite very different wind forcing (Fig. 2), is due to the models’ making two large opposing errors which balance each other. One of the errors associated with model-underestimated wind intensification is caused by the absence of the related surface cooling in the models (Fig. 4). The other, compensating, error, has to do with nonlinear dynamics of ocean-eddy response to the changing wind input (Fig. 3), since these ocean eddies are grossly under-resolved in the current generation of climate general circulation models (GCMs)." @default.
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- W134202456 date "2010-05-01" @default.
- W134202456 modified "2023-09-23" @default.
- W134202456 title "Mesoscale Ocean Eddies and Climate Change over the Southern Ocean" @default.
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