Titlebook: Wave Packets and Their Bifurcations in Geophysical Fluid Dynamics; Huijun Yang Book 1991 Springer-Verlag New York 1991 Meteorology.Ocean.O

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Evolution of Wave Packets in Stratified Baroclinic Basic Flow,flow is of great importance in geophysical fluids. Therefore, in this chapter we extend the previous results (Yang, 1988b,c) into a three-dimensional disturbance system with the baroclinic basic flow. The vorticity equation of motion and Ertel theorem are given in Section 7.2. The model is a three-d

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Book 1991 other monographs. The investigation of wave packets and their bi­ furcations is very interesting, and useful theoretically and in practice, not only in geophysical fluid dynamics, which is the field to which the theory is being applied here, but also in other fields in mathematics and the natural s

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Evolution of Wave Packets in Stratified Baroclinic Basic Flow,atified geophysical flow is derived in Section 7.3. The equations determining the structure and its change are addressed in Section 7.4. Integral properties of this model are presented in Section 7.5. Sections 7.6 and 7.7 discuss the structures of wave packets and their changes on the zonal and meridional basic flow, respectively.

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Evolution of Wave Packets in Stratified Baroclinic Basic Flow,atified geophysical flow is derived in Section 7.3. The equations determining the structure and its change are addressed in Section 7.4. Integral properties of this model are presented in Section 7.5. Sections 7.6 and 7.7 discuss the structures of wave packets and their changes on the zonal and meridional basic flow, respectively.

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