Baroclinic solitary Rossby waves in an N-level model
N层模式大气中的斜压孤立Rossby波

The KdV equation is derived from a N-level model. The streamline patterns of solitary Rossby waves are calculated with a three-level model. The results show that the influence of the vertical and horizontal shears of the basic flow and Froude number on the solitary Rossby waves is quite important. The streamline patterns of the solitary waves with different modes are different.