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...
| Päätekijät: | , |
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| Aineistotyyppi: | Journal article |
| Kieli: | English |
| Julkaistu: |
2009
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