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OA Marine2
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Copernicus Publications2
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✓Ocean Science2
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20161
20141
D. Rayner results 2 · Newest (Page 1/1, per page 25)
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Journal: Ocean Science ×Author: D. Rayner ×Clear All Filters
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Compensation between meridional flow components of the Atlantic MOC at 26° NOA Marine
Ocean Science · 2016 · Vol. 12 · Issue 2 · Copernicus Publications / European Geosciences Union
E. Frajka-Williams; C. S. Meinen; W. E. Johns; D. A. Smeed; A. Duchez; A. J. Lawrence; D. A. Cuthbertson; G. D. McCarthy; H. L. Bryden; M. O. Baringer; B. I. Moat; D. Rayner
From ten years of observations of the Atlantic meridional overturning circulation (MOC) at 26° N (2004–2014), we revisit the question of flow compensation between components of the circulation. Contrasting with early results from the observations, transport variations of the Florida Current (FC) and upper mid-ocean (UMO) transports (top 1000 m east of the Bahamas) are now found to compensate on sub-annual timescales. The obser...
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Observed decline of the Atlantic meridional overturning circulation 2004–2012OA Marine
Ocean Science · 2014 · Vol. 10 · Issue 1 · Copernicus Publications / European Geosciences Union
D. A. Smeed; G. D. McCarthy; S. A. Cunningham; E. Frajka-Williams; D. Rayner; W. E. Johns; C. S. Meinen; M. O. Baringer; B. I. Moat; A. Duchez; H. L. Bryden
The Atlantic meridional overturning circulation (AMOC) has been observed continuously at 26° N since April 2004. The AMOC and its component parts are monitored by combining a transatlantic array of moored instruments with submarine-cable-based measurements of the Gulf Stream and satellite derived Ekman transport. The time series has recently been extended to October 2012 and the results show a downward trend since 2004. From A...
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