The Salinity, Heat, and Buoyancy Budgets of a Coastal Current in a Marginal Sea
The Atlantic overturning circulation has conventionally been pictured in the meridional-vertical plane, but a significant densification of the water masses involved also occurs as the surface branch of the circulation flows in boundary currents around the subpolar gyre and northern marginal seas. He...
Egile Nagusiak: | Wahlin, A, Johnson, H |
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Formatua: | Journal article |
Hizkuntza: | English |
Argitaratua: |
2009
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