摘要
本文通过一次西太平洋副高进退过程的分析得到,海上西太平洋副高主体和大陆西太副高(脊)维持的环流机制是不同的。前者和经典的环流模式一致。后者和经典模式不同,推断主要受副副热带季风环流的作用,并且副热带季风环流有超前副高进退的指示意义。
In this paper, a diagnostic analysis of advance and retreat of the West Pacific subtropical high suggests different circulation mechanisms acting on its maritime main body and continental ridge extension.The former is consistent with classic circulation model while the latter differs from it. It is inferred that the ridge is subject to subtropical monsoon circulation, which is early indicative of the advance and retreat of the high.
出处
《热带气象》
CSCD
1989年第3期220-226,共7页
基金
国家自然科学基金资助项目
