摘要
Ⅰ. INTRODUCTION In recent years, many synoptic facts show that the effect of cross-equatorial current from one hemisphere to the other on the general circulation is very important. In summer, such effect on the formation of Asian monsoon circulation over West Indian Ocean (Somali Jet) is obvious. In this paper, by use of simulation in a rotating annulus experiment, the effect of the cross-equatorial current as a
