Articles | Volume 12, issue 2
Ocean Sci., 12, 481–493, 2016
Ocean Sci., 12, 481–493, 2016

Research article 01 Apr 2016

Research article | 01 Apr 2016

Compensation between meridional flow components of the Atlantic MOC at 26° N

E. Frajka-Williams et al.


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Eleanor Frajka-Williams on behalf of the Authors (08 Mar 2016)  Author's response
ED: Publish subject to technical corrections (17 Mar 2016) by Mario Hoppema
Short summary
The ocean meridional overturning circulation (MOC) is predicted by climate models to slow down in this century, resulting in reduced transport of heat northward to mid-latitudes. At 26° N, the Atlantic MOC has been measured continuously for the past decade (2004–2014). In this paper, we discuss the 10-year record of variability, identify the origins of the continued weakening of the circulation, and discuss high-frequency (subannual) compensation between transport components.