摘要
In this paper,using a nonlinear low-order barotropic system with orography and momentum forcing as well as dissipation,we have theoretically calculated the two kinds of curves for the seasonal northward movement of subtropical highs.It has been shown that the theoretical results resemble basically with the analysed results of wave spectrum data.
In this paper,using a nonlinear low-order barotropic system with orography and momentum forcing as well as dissipation,we have theoretically calculated the two kinds of curves for the seasonal northward movement of subtropical highs.It has been shown that the theoretical results resemble basically with the analysed results of wave spectrum data.
