| Summary |
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| • | Circulation shows
some comparison with present |
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| understanding of
circulation |
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| • | Surface
temperature compares well to observations |
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| • | Mixed layer
follows realistic seasonal patterns, although |
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| is too deep in
winter |
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| • | Onshore flux of
CDW occurs at observed locations |
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| • | Onshore flux due
to combination of bathymetric |
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| curvature and
shelf circulation |
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