The North Atlantic Ocean Is in a State of Reduced Overturning
Abstract The Atlantic Meridional Overturning Circulation (AMOC) is responsible for a variable and climatically important northward transport of heat. Using data from an array of instruments that span the Atlantic at 26°N, we show that the AMOC has been in a state of reduced overturning since 2008 as...
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| Główni autorzy: | , , , , , , , , , , |
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| Format: | Artigo |
| Język: | Inglês |
| Wydane: |
Wiley
2018-02-01
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| Seria: | Geophysical Research Letters |
| Hasła przedmiotowe: | |
| Dostęp online: | https://doi.org/10.1002/2017GL076350 |
| Etykiety: |
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