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Baroclinic Instability of Two-Layer Flows over One-Dimensional Bottom Topography
Baroclinic Instability Two-Layer Flows One-Dimensional Bottom Topography
2008/8/7
Using the QG approximation, the stability of two-layer zonal flows on the beta plane over bottom topography is examined. The topography is assumed to be one-dimensional, with the isobaths being direct...