The Irminger Gyre as a Key Driver of the Subpolar North Atlantic Overturning
Abstract The lower limb of the Atlantic meridional overturning circulation (AMOC) is the equatorward flow of dense waters formed through the cooling and freshening of the poleward‐flowing upper limb. In the subpolar North Atlantic (SPNA), upper limb variability is primarily set by the North Atlantic...
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| Автори: | , , , , , , , , , |
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| Формат: | Artigo |
| Мова: | Inglês |
| Опубліковано: |
Wiley
2024-04-01
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| Серія: | Geophysical Research Letters |
| Онлайн доступ: | https://doi.org/10.1029/2024GL108457 |
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