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Article Dans Une Revue Nonlinear Processes in Geophysics Année : 1998

The nonlinear evolution of unstable coupled equatorial ocean-atmosphere modes

Résumé

In this paper we investigate whether observed intraseasonal variability in the equatorial Pacific can be attributed to finite amplitude waves resulting from unstable air-sea interactions. Within a Zebiak - Cane type model of the coupled equatorial ocean - atmosphere, the nonlinear equilibration of instabilities of a simple basic state is considered with periodic conditions on the ocean boundaries. Three mechanisms exist which can induce a finite amplitude equilibration on a time scale ?2t. Here t is the characteristic time scale of growth of the disturbance and ? the relative distance from the instability threshold. For each equilibration mechanism, the finite amplitude and period of the equilibrium state are computed as a function of ? and substantial amplitude can be reached for a reasonable degree of supercriticality. Thereafter the analysis is extended to include time-dependent external forcing. It is shown that interannual variability may result through the interaction of the response of a weak annual external forcing and the finite amplitude development of the intraseasonal instabilities.
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Dates et versions

hal-00301881 , version 1 (18-06-2008)

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  • HAL Id : hal-00301881 , version 1

Citer

P. C. F. van Der Vaart, H. A. Dijkstra. The nonlinear evolution of unstable coupled equatorial ocean-atmosphere modes. Nonlinear Processes in Geophysics, 1998, 5 (1), pp.39-52. ⟨hal-00301881⟩
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