What causes the location of the air-sea turbulent heat flux maximum over the Labrador Sea?
The Labrador Sea is a region of climatic importance as a result of the occurrence of oceanic wintertime convection, a process that is integral to the Atlantic Meridional Overturning Circulation. This process requires large air-sea heat fluxes that result in a loss of surface buoyancy, triggering con...
| Published in: | Geophysical Research Letters |
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| Main Authors: | , , , |
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
| Published: |
2014
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| Subjects: | |
| Online Access: | https://ueaeprints.uea.ac.uk/id/eprint/48833/ https://doi.org/10.1002/2014GL059940 |