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本文在半地转概念下，讨论了线性和非线性地形罗斯贝波的稳定性及其解。
The stability and the solutions of linear and nonlinear topographically generated Rossby Waves were discussed by using a barotropic semi-geostrophic model.
正压和赤道斜压罗斯·贝波的非线性相互作用。
The Nonlinear Interaction of Barotropic and Equatorial Baroclinic Rossby Waves.
对比副热带急流所生罗斯·贝波变形半径，阐明海洋天气式涡旋小于和慢于大气中的数十倍。
As compared with Rossby deformation radius in atmospheric jet current synoptic eddies in ocean are ten times as small in their dimensions and ten times as slow as those in atmosphere.
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