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Chapter ShallowWaterEquationsandtheOcean Over most of the glob e the o cean has a rather distinctive vertical structure with an upp er layer ranging from m to m in thickness consisting of water heat

The water in this upp er layer is therefore less dense than deep o cean water This density stratication is weak or absent only in certain highlatitude regions of the North Atlantic and in a few other lo cations In these regions surface water has b e

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Chapter ShallowWaterEquationsandtheOcean Over most of the glob e the o cean has a rather distinctive vertical structure with an upp er layer ranging from m to m in thickness consisting of water heat






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