Oceanic warming of western Europe
In the northern North Atlantic off Europe, deep convection flushes buoyancy and heat out of the upper ocean each winter. It is replaced by horizontal advection during the remainder of the year. Absolute geostrophic currents can be computed from an application of the heat conservation equation. A rem...
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| Udgivet i: | Proc Natl Acad Sci U S A |
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| Hovedforfatter: | |
| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
National Academy of Sciences
1979
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| Fag: | |
| Online adgang: | https://ncbi.nlm.nih.govhttps://pmc.ncbi.nlm.nih.gov/articles/PMC383638/ https://ncbi.nlm.nih.govhttps://pubmed.ncbi.nlm.nih.gov/16592662/ https://ncbi.nlm.nih.govhttps://doi.org/10.1073/pnas.76.6.2518 |
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