摘要
A weak nonlinear model of a two-layer barotropic ocean with Rayleigh dissipation is built. The analytic asymptotic solution is derived in the mid-latitude stationary wind field, and the physical meaning of the corresponding problem is discussed.
- 出版日期2013-3
- 单位安徽师范大学; 中国科学院大气物理研究所; 中国科学院大学