The North Atlantic Ocean Is in a State of Reduced Overturning

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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Bibliographic Details
Main Authors: D. A. Smeed, S. A. Josey, C. Beaulieu, W. E. Johns, B. I. Moat, E. Frajka‐Williams, D. Rayner, C. S. Meinen, M. O. Baringer, H. L. Bryden, G. D. McCarthy
Format: Article
Language:English
Published: Wiley 2018-02-01
Series:Geophysical Research Letters
Subjects:
Atlantic
AMOC
overturning
circulation
Online Access:https://doi.org/10.1002/2017GL076350
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https://doi.org/10.1002/2017GL076350

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