Baroclinic stability of oceanic long Rossby wave in the North Pacific Subtropical Countercurrent;

Application of Jacobi elliptic functions in the atmospheric and oceanic dynamics: studies on two-dimensional nonlinear Rossby waves;

Computational properties of a new horizontal staggered grid for Rossby waves;

Exact solutions to the nonlinear Rossby waves with a complete representation of the Coriolis force;

Effects of the Horizontal Component of the Earth’s Rotation on Rossby Waves;

It is shown that the Rossby waves possess a tilting spiral structure, which represents that the stream field is horizontal convergence at lower layer and ascendi.

SASWJ exhibits changes of jet axis,intension and Rossby wave activity along SASWJ,and perturbation kinetic energy index along SASWJ can indicate Asia jet variability.

It is found by the WKB method that the packetof nonlinear Vortex Rossby wave which is effected by Rossby parameterβisgoverned by the nonlinear Schr(?)dinger equation and we solve the Schr(?)dingerequation under the condition that has practi.

This is exactly the physical sources of vortex Rossby wave.

The principal band caused by vortex Rossby waves is related well to the 850hPa positive vorticity band and has heavy rainfall.

The analytic solution is similar to the propagating vortex Rossby waves(VRW) due to the topographic βeff takes effects resemble with the radial derivative of basic-state vertical vorticity of tropical cyclone.

A high resolution shallow-water model is designed to study the roles which the topographical parameter and latitudinal basic flow play in the propagation of vortex Rossby waves and typhoon tangential velocity changes.