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...

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Egile Nagusiak: Wahlin, A, Johnson, H
Formatua: Journal article
Hizkuntza:English
Argitaratua: 2009

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