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Ocean Science An interactive open-access journal of the European Geosciences Union
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Volume 10, issue 4
Ocean Sci., 10, 601–609, 2014
https://doi.org/10.5194/os-10-601-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
Ocean Sci., 10, 601–609, 2014
https://doi.org/10.5194/os-10-601-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 03 Jul 2014

Research article | 03 Jul 2014

An observed 20-year time series of Agulhas leakage

D. Le Bars1, J. V. Durgadoo2, H. A. Dijkstra1, A. Biastoch2, and W. P. M. De Ruijter1 D. Le Bars et al.
  • 1IMAU, Utrecht University, P.O. Box 80.005, 3508 TA Utrecht, The Netherlands
  • 2GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany

Abstract. We provide a time series of Agulhas leakage anomalies over the last 20-years from satellite altimetry. Until now, measuring the interannual variability of Indo-Atlantic exchange has been the major barrier in the investigation of the dynamics and large scale impact of Agulhas leakage. We compute the difference of transport between the Agulhas Current and Agulhas Return Current, which allows us to deduce Agulhas leakage. The main difficulty is to separate the Agulhas Return Current from the southern limb of the subtropical "supergyre" south of Africa. For this purpose, an algorithm that uses absolute dynamic topography data is developed. The algorithm is applied to a state-of-the-art ocean model. The comparison with a Lagrangian method to measure the leakage allows us to validate the new method. An important result is that it is possible to measure Agulhas leakage in this model using the velocity field along a section that crosses both the Agulhas Current and the Agulhas Return Current. In the model a good correlation is found between measuring leakage using the full depth velocities and using only the surface geostrophic velocities. This allows us to extend the method to along-track absolute dynamic topography from satellites. It is shown that the accuracy of the mean dynamic topography does not allow us to determine the mean leakage but that leakage anomalies can be accurately computed.

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