%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES
%A Loveday, B. R.
%A Durgadoo, J. V.
%A Reason, C. J. C.
%A Biastoch, A.
%A Penven, Pierrick
%T Decoupling of the Agulhas leakage from the Agulhas Current
%D 2014
%L fdi:010062384
%G ENG
%J Journal of Physical Oceanography
%@ 0022-3670
%K OCEAN INDIEN ; ATLANTIQUE SUD
%M ISI:000339183800006
%N 7
%P 1776-1797
%R 10.1175/jpo-d-13-093.1
%U https://www.documentation.ird.fr/hor/fdi:010062384
%> https://www.documentation.ird.fr/intranet/publi/2014/08/010062384.pdf
%V 44
%W Horizon (IRD)
%X The relationship between the Agulhas Current and the Agulhas leakage is not well understood. Here, this is investigated using two basin-scale and two global ocean models of incrementally increasing resolution. The response of the Agulhas Current is evaluated under a series of sensitivity experiments, in which idealized anomalies, designed to geometrically modulate zonal trade wind stress, are applied across the Indian Ocean Basin. The imposed wind stress changes exceed plus or minus two standard deviations from the annual-mean trade winds and, in the case of intensification, are partially representative of recently observed trends. The Agulhas leakage is quantified using complimentary techniques based on Lagrangian virtual floats and Eulerian passive tracer flux. As resolution increases, model behavior converges and the sensitivity of the leakage to Agulhas Current transport anomalies is reduced. In the two eddy-resolving configurations tested, the leakage is insensitive to changes in Agulhas Current transport at 328S, though substantial eddy kinetic energy anomalies are evident. Consistent with observations, the position of the retroflection remains stable. The decoupling of Agulhas Current variability from the Agulhas leakage suggests that while correlations between the two may exist, they may not have a clear dynamical basis. It is suggested that present and future Agulhas leakage proxies should be considered in the context of potentially transient forcing regimes.
%$ 032