Models for instability in geophysical flows
The generation of instability in inviscid, non-diffusive geophysical flows is generically caused by a resonance between two wave modes. The weakly nonlinear unfolding of this situation is described in the long-wave regime, using a particular two-layer quasi-geostrophic model as an illustrative examp...
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Main Authors: | , |
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Format: | Default Preprint |
Published: |
2000
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Subjects: | |
Online Access: | https://hdl.handle.net/2134/765 |
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