Simulation of planetary wave breaking and polar vortex erosion in the stratosphere has been carried out using three different global shallow water numerical models.The models are an Eulerian spectral model, a semi-Lagrangian finite difference mode1 based on a vector discretization of the momentum equation and a semi-Lagrangian finite difference mode1 based on the potential vorticity and divergence equations.The results of the integrations indicate advantages of the potential vorticity-based mode1 in the vortex erosion problem.RSUM On utilise trois modles numen'ques mondiaux bass sur les equations de St-Venant pour simuler le dferlement d'ondes plantaires et l'rosion de la circulation polaire dans la stratosphre: le modele spectral eulrien; le modle diffrences finies semi-lagrangien bas sur une discretisation vectorielle de l'equation de la quantit de mouvement; et le modle d dtf&rences fnies semi-lagrangien bas sur les equations du tourbillon potentiel et de la divergence.Les rsultats des integrations indiquent les avantages du modele bas sur le tourbillon potentiel dans le problme de l'rosion de la circulation.
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Bates et al. (1997) studied this question.
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