{"refrec":{"BRefID":113642,"RR":"<b>Kanzow, T.; Cunningham, S.A.; Rayner, D.; Hirschi, J.J.-M.; Johns, W.E.; Baringer, M.O.; Bryden, H.L.; Beal, L.M.; Meinen, C.S.; Marotzke, J.</b> (2007). Observed flow compensation associated with the MOC at 26.5°N in the Atlantic. <i>Science (Wash.) 317(5840)</i>: 938-941","BEntID":108096,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 317(5840)</i>: 938-941","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Kanzow, T.; Cunningham, S.A.; Rayner, D.; Hirschi, J.J.-M.; Johns, W.E.; Baringer, M.O.; Bryden, H.L.; Beal, L.M.; Meinen, C.S.; Marotzke, J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Kanzow, T. <i>et al.</i>","Englishabstract":"The Atlantic meridional overturning circulation (MOC), which provides one-quarter of the global meridional heat transport, is composed of a number of separate flow components. How changes in the strength of each of those components may affect that of the others has been unclear because of a lack of adequate data. We continuously observed the MOC at 26.5°N for 1 year using end-point measurements of density, bottom pressure, and ocean currents; cable measurements across the Straits of Florida; and wind stress. The different transport components largely compensate for each other, thus confirming the validity of our monitoring approach. The MOC varied over the period of observation by ±5.7 x 10<sup>6</sup> cubic meters per second, with density-inferred and wind-driven transports contributing equally to it. 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