1) Barotropic Rossby waves
正压Rossby波
2) the first baroclinic Rossby wave
第一斜压Rossby波
1.
Based on the linear free Rossby wave theory in the stratified fluid,the first baroclinic Rossby wave phase speed can be given by β λ~2_1,so the times for the first baroclinic Rossby wave to cross different ocean basins can be computed from respective ocean basin widths.
根据层结流体中线性自由Rossby波理论,可知第一斜压Rossby波位相速度为βλ21,故由全球各个大洋海盆的宽度可得到第一斜压Rossby波在各大洋海盆中从东边界传到西边界的时间。
3) the first mode baroclinic Rossby wave
第一斜压模Rossby波
4) the second mode baroclinic Rossby wave
第二斜压模Rossby波
5) rossby wave
Rossby波
1.
Baroclinic stability of oceanic long Rossby wave in the North Pacific Subtropical Countercurrent;
北太平洋副热带向东逆流区Rossby波斜压稳定性
2.
Application of Jacobi elliptic functions in the atmospheric and oceanic dynamics: studies on two-dimensional nonlinear Rossby waves;
雅可比椭圆函数在大气和海洋动力学中的应用:二维非线性Rossby波研究
3.
Computational properties of a new horizontal staggered grid for Rossby waves;
一种新水平网格的Rossby波计算特性
6) Rossby waves
Rossby波
1.
Exact solutions to the nonlinear Rossby waves with a complete representation of the Coriolis force;
完整Coriolis力作用下非线性Rossby波的精确解
2.
Effects of the Horizontal Component of the Earth’s Rotation on Rossby Waves;
地球旋转水平分量对Rossby波的影响
3.
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.
应用描写大气大尺度运动的准地转方程组 ,求得了大气Rossby波的三维定常流场以及相应的位温场、涡度场和散度场 ,其中的三维流场构成了物理空间的一个非线性自治动力系统 。
补充资料：冲击波超压与动压