Entrainment in the Denmark Strait overflow plume by meso-scale eddies
The entrainment of buoyant ambient water into the overflow plume of Denmark Strait and the associated downstream warming of the plume are estimated using time series of currents and temperature from moored instrumentation and classical hydrographic data. Warming rates are highest (0.4–0.5 K/100 km)...
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| Auteurs principaux: | , |
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| Format: | Artigo |
| Langue: | Inglês |
| Publié: |
Copernicus Publications
2010-03-01
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| Collection: | Ocean Science |
| Accès en ligne: | http://www.ocean-sci.net/6/301/2010/os-6-301-2010.pdf |
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