Three-dimensional reconstruction of oceanic mesoscale currents from surface information

International audience The ability to reconstruct the three‐dimensional (3D) dynamics of the ocean by an effective version of Surface Quasi‐Geostrophy (eSQG) is examined. Using the fact that surface density plays an analogous role as interior potential vorticity (PV), the eSQG method consists in inv...

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Bibliographic Details
Published in:Journal of Geophysical Research
Main Authors: Capet, Xavier, Hua, Bach Lien, Mcwilliams, James C., Isern-Fontanet, Jordi, Lapeyre, Guillaume, Klein, Patrice, Chapron, Bertrand, Hecht, Matthew
Other Authors: Laboratoire de physique des océans (LPO), Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS), Department of Atmospheric Sciences Los Angeles, University of California Los Angeles (UCLA), University of California (UC)-University of California (UC), Laboratoire d'Océanographie Spatiale (LOS), Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER), Laboratoire de Météorologie Dynamique (UMR 8539) (LMD), Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL), Los Alamos National Laboratory (LANL)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2008
Subjects:
SST
Online Access:https://hal.science/hal-02051290
https://hal.science/hal-02051290/document
https://hal.science/hal-02051290/file/2007JC004692.pdf
https://doi.org/10.1029/2007JC004692
Description
Summary:International audience The ability to reconstruct the three‐dimensional (3D) dynamics of the ocean by an effective version of Surface Quasi‐Geostrophy (eSQG) is examined. Using the fact that surface density plays an analogous role as interior potential vorticity (PV), the eSQG method consists in inverting the QG PV generated by sea‐surface density only. We also make the extra assumption that sea‐surface temperature (SST) anomalies fully represent surface density anomalies. This approach requires a single snapshot of SST and the setup of two parameters: the mean Brunt‐Väisälä frequency and a parameter that determines the energy level at the ocean surface. The validity of this approach is tested using an Ocean General Circulation Model simulation representing the North Atlantic in winter. It is shown that the method is quite successful in reconstructing the velocity field at the ocean surface for mesoscales (between 30 and 300 km). The eSQG framework can also be applied to reconstruct subsurface fields using surface information. Results show that the reconstruction of velocities and vorticity from surface fields is reasonably good for the upper 500 m and that the success of the method mainly depends on the quality of the SST as a proxy of the density anomaly at the base of the mixed layer. This situation happens after a mixed‐layer deepening period. Therefore the ideal situation for the application of this method would be after strong wind events.