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Ocean Science An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 5
Ocean Sci., 9, 825-835, 2013
https://doi.org/10.5194/os-9-825-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
Ocean Sci., 9, 825-835, 2013
https://doi.org/10.5194/os-9-825-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 23 Sep 2013

Research article | 23 Sep 2013

Transport of Antarctic bottom water through the Kane Gap, tropical NE Atlantic Ocean

E. G. Morozov1, R. Y. Tarakanov1, and H. van Haren2 E. G. Morozov et al.
  • 1Shirshov Institute of Oceanology, Russian Academy of Sciences, Nakhimovsky pr. 36, Moscow, 117997, Russia
  • 2Royal Netherlands Institute for Sea Research (NIOZ), P.O. Box 59, 1790 AB, Den Burg, the Netherlands

Abstract. We study low-frequency properties of the Antarctic Bottom Water (AABW) flow through the Kane Gap (9° N) in the Atlantic Ocean. The measurements in the Kane Gap include five visits with CTD (Conductivity-Temperature-Depth) sections in 2009–2012 and a year-long record of currents on a mooring using three AquaDopp current meters. We found an alternating regime of flow, which changes direction several times during a year. The seasonal signal seems to dominate. The maximum daily average values of southerly velocities reach 0.20 m s−1, while the greatest north-northwesterly velocity is as high as 0.15 m s−1. The velocity and transport at the bottom are aligned along the slope of a local hill near the southwestern side of the gap. The distribution of velocity directions at the upper boundary of AABW is wider. The transport of AABW (Θ < 1.9 °C) based on the mooring and LADCP (Lowered Acoustic Doppler Current Profiler) data varies approximately within ±0.35 Sv in the northern and southern directions. The annual mean AABW transport through the Kane Gap is almost zero.

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