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      Continuous, Array-Based Estimates of Atlantic Ocean Heat Transport at 26.5°N

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          Improved Global Sea Surface Temperature Analyses Using Optimum Interpolation

          Richard Reynolds, Thomas M Smith (1994)
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            A signature of persistent natural thermohaline circulation cycles in observed climate

            Jeff Knight (2005)
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              Temporal variability of the Atlantic meridional overturning circulation at 26.5 degrees N.

              Stuart A Cunningham, Torsten Kanzow, Darren Rayner … (2007)
              The vigor of Atlantic meridional overturning circulation (MOC) is thought to be vulnerable to global warming, but its short-term temporal variability is unknown so changes inferred from sparse observations on the decadal time scale of recent climate change are uncertain. We combine continuous measurements of the MOC (beginning in 2004) using the purposefully designed transatlantic Rapid Climate Change array of moored instruments deployed along 26.5 degrees N, with time series of Gulf Stream transport and surface-layer Ekman transport to quantify its intra-annual variability. The year-long average overturning is 18.7 +/- 5.6 sverdrups (Sv) (range: 4.0 to 34.9 Sv, where 1 Sv = a flow of ocean water of 10(6) cubic meters per second). Interannual changes in the overturning can be monitored with a resolution of 1.5 Sv.
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                Author and article information

                Journal
                Title: Journal of Climate
                Abbreviated Title: J. Climate
                Publisher: American Meteorological Society
                ISSN (Print): 0894-8755
                ISSN (Electronic): 1520-0442
                Publication date Created: May 2011
                Publication date (Print): May 2011
                Volume: 24
                Issue: 10
                Pages: 2429-2449
                Article
                DOI: 10.1175/2010JCLI3997.1
                SO-VID: e51da439-0abd-4d87-a0ff-cf7eb79c209a
                Copyright © © 2011
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