Evolution of a barotropic shear layer into elliptical vortices

Anirban Guha1, Mona Rahmani, Gregory A Lawrence

  • 1Department of Civil Engineering, University of British Columbia, Vancouver, Canada V6T 1Z4. aguha@mail.ubc.ca

Summary

A piecewise linear shear layer generates unique elliptical vortices via Kelvin-Helmholtz instability (KHI). This KHI arises from interacting counterpropagating vorticity waves, explaining vortex formation in planetary atmospheres and oceans.

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