Publications des scientifiques de l'IRD

Renault L., McWilliams J. C., Penven Pierrick. (2017). Modulation of the Agulhas Current retroflection and leakage by oceanic current interaction with the atmosphere in coupled simulations [+ Corrigendum]. Journal of Physical Oceanography, 47 (8), p. 2077-2100 [+ Corrigendum in : Journal of Physical Oceanography, 48 (4), p. 1009 p. 1009]. ISSN 0022-3670.

Titre du document
Modulation of the Agulhas Current retroflection and leakage by oceanic current interaction with the atmosphere in coupled simulations [+ Corrigendum]
Année de publication
2017
Type de document
Article référencé dans le Web of Science WOS:000407420500011
Auteurs
Renault L., McWilliams J. C., Penven Pierrick
Source
Journal of Physical Oceanography, 2017, 47 (8), p. 2077-2100 [+ Corrigendum in : Journal of Physical Oceanography, 48 (4), p. 1009 p. 1009] ISSN 0022-3670
Coupled ocean-atmosphere simulations are carried out for the Mozambique Channel, the Agulhas Current system, and the Benguela upwelling system to assess the ocean surface current feedback to the atmosphere and its impact on the Agulhas Current (AC) retroflection and leakage. Consistent with previous studies, the authors show that the current feedback slows down the oceanic mean circulation and acts as an oceanic eddy killer by modulating the energy transfer between the atmosphere and the ocean, reducing by 25% the mesoscale energy and inducing a pathway of energy transfer from the ocean to the atmosphere. The current feedback, by dampening the eddy kinetic energy (EKE), shifts westward the distribution of the AC retroflection location, reducing the presence of eastern retroflections in the simulations and improving the realism of the AC simulation. By modulating the EKE, the AC retroflection and the Good Hope jet intensity, the current feedback allows a larger AC leakage (by 21%), altering the water masses of the Benguela system. Additionally, the eddy shedding is shifted northward and the Agulhas rings propagate less far north in the Atlantic. The current-wind coupling coefficient s(w) is not spatially constant: a deeper marine boundary layer induces a weaker s(w). Finally the results indicate that the submesoscale currents may also be weakened by the current feedback.
Plan de classement
Sciences fondamentales / Techniques d'analyse et de recherche [020] ; Limnologie physique / Océanographie physique [032]
Description Géographique
AFRIQUE DU SUD ; OCEAN INDIEN ; ATLANTIQUE ; MADAGASCAR ; BENGUELA
Localisation
Fonds IRD [F B010070959]
Identifiant IRD
fdi:010070959
Contact