Journal of Environmental Waste Management and Recycling

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Eddies Open Access Journals

The ability to parameterize Ocean eddy effects in an affected coarse-resolution ocean general circulation model is assessed. The immanent form results in a suite of different ocean wind stress cause distract is presented and compared to identical experiments performed with the same model in 0.1° eddy-resolving resolution. With forcing of nowadays wind stress property and a thickness diffusivity formulated in terms of the local stratification it is shown that the Southern Ocean residual meridional overturning circulation in the two models is different in structure and magnitude. It is found that the difference in the upper overturning cell is primarily explained by an overly strong subsurface flow in the parameterized eddy-induced circulation while the difference in the lower cell is mainly evaluated to the mean-flow overturning.

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