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On the Influence of the Current Feedback to the Atmosphere on the Western Mediterranean Sea Dynamics
Author(s) -
Renault L.,
Arsouze T.,
BallabreraPoy J.
Publication year - 2021
Publication title -
journal of geophysical research: oceans
Language(s) - English
Resource type - Journals
eISSN - 2169-9291
pISSN - 2169-9275
DOI - 10.1029/2020jc016664
Subject(s) - ocean gyre , mesoscale meteorology , ocean current , atmosphere (unit) , environmental science , climatology , baroclinity , eddy , mediterranean sea , geology , atmospheric sciences , mechanics , turbulence , meteorology , physics , mediterranean climate , geography , subtropics , archaeology , fishery , biology
The ocean Current FeedBack to the atmosphere (CFB) has been shown to be an unambiguous physical process to achieve proper equilibrium in the Ocean. However, its effects on the Western Mediterranean Sea (WMS) are not known. In this study, eddy‐rich coupled ocean‐atmosphere simulations are carried out for the WMS to assess the extent to which CFB alters the WMS circulation and to characterize the low‐level wind and surface stress responses to CFB. By generating conduits of energy from oceanic currents to the atmosphere, CFB slows the mean circulation by about 10% and acts as an oceanic eddy killer, reducing the mesoscale activity by 25% and attenuating the intensity of their intermittency. It also alters the mean barotropic vorticity balance of the WMS Gyre, reducing the role of wind stress curl, nonlinear torque, and bottom pressure torque. By reducing the eddy‐mean flow interaction, CFB has a large influence on the properties of the Algerian Current, reducing the presence of standing eddies near Sardinia and improving the realism of the circulation. It also modifies the Alboran Gyres formation and the Northern Current retroflection. Finally, coupling coefficients from the coupled simulations are estimated and are consistent with those for other regions. The CFB coupling coefficients can be used to parameterize the CFB in a forced ocean model. Overall, our results show that, as for other regions, the CFB is another physical mechanism to be considered for the representation of the WMS circulation.