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AGU: Journal of Geophysical Research, Oceans

 

Keywords

  • Oceanic eddies
  • regional modeling
  • wavelet analysis
  • Agulhas current system
  • Southeast Atlantic ocean

Index Terms

  • Oceanography: General: Numerical modeling
  • Oceanography: Physical: Eddies and mesoscale processes
  • Oceanography: Physical: General circulation
Abstract
Cited By (0)
 

Abstract

Tracking coherent structures in a regional ocean model with wavelet analysis: Application to Cape Basin eddies

A. M. Doglioli

Laboratoire de Physique des Océans, UMR 6523 CNRS/IFREMER/UBO, Brest, France

B. Blanke

Laboratoire de Physique des Océans, UMR 6523 CNRS/IFREMER/UBO, Brest, France

S. Speich

Laboratoire de Physique des Océans, UMR 6523 CNRS/IFREMER/UBO, Brest, France

G. Lapeyre

Laboratoire de Météorologie Dynamique IPSL, École Normale Supérieure/CNRS, Paris, France

This study is mainly aimed at proposing objective tools for the identification and tracking of three-dimensional eddy structures. It is conducted with a high-resolution numerical model of the ocean region around South Africa, and emphasis is put on Cape Basin anticyclones and cyclones thought to be actively implicated in the Indian-Atlantic interocean exchange. We settle on wavelet analysis for the decomposition and processing of successive maps of relative vorticity for a simulation run with inline equation° resolution. The identification of three-dimensional coherent structures comes with the calculation of eddy trajectories and the time evolution of eddy properties. Instantaneous mass transport and momentum of eddies are calculated from the knowledge of instantaneous drift velocities, volumes, and diameters. The success of the regional model and of the analysis technique is assessed through comparisons with equivalent observations.

Received 13 October 2006; accepted 29 January 2007; published 23 May 2007.

Citation: Doglioli, A. M., B. Blanke, S. Speich, and G. Lapeyre (2007), Tracking coherent structures in a regional ocean model with wavelet analysis: Application to Cape Basin eddies, J. Geophys. Res., 112, C05043, doi:10.1029/2006JC003952.

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