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The response of a simple quasi-unidimensional barotropic model is studied. Wave-wave interaction, and bending the linear resonant response to the topographic forcing allows multiple equilibria if the zonal mean flow is assigned. The stationary solutions corresponding to the equilibria are compared with the observations.
The response of a simple quasi-unidimensional barotropic model is studied. Wave-wave interaction, and bending the linear resonant response to the topographic forcing allows multiple equilibria if the zonal mean flow is assigned. The stationary solutions corresponding to the equilibria are compared with the observations.
| All Time | Past Year | Past 30 Days | |
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| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 167 | 18 | 1 |
| PDF Downloads | 20 | 12 | 0 |
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