Thursday, 16 June 2005: 10:50 AM
Ballroom A (Hyatt Regency Cambridge, MA)
Coherent vortices are an important component of the mesoscale eddy variability of the ocean. Here we investigate the interaction of three-dimensional quasigeostrophic (qg) vortices in the ellipsoidal moment approximation and compare with simulations of the qg fluid equations. We find a clear separation between the process of merger and alignment. Merger corresponds to a transition to strong chaos, while alignment is a more subtle phenomenon involving vortex Rossby waves.
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