| 一次西太平洋副高中期进退过程环流机制的分析 |
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| 引用本文： | 喻世华,潘春生.一次西太平洋副高中期进退过程环流机制的分析[J].热带气象学报,1989,0(3):220-226. |
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| 作者姓名： | 喻世华 潘春生 |
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| 作者单位： | 空军气象学院 |
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| 基金项目： | 国家自然科学基金资助项目 |
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| 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。
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| 收稿时间： | 1988/3/23 0:00:00 |
| 修稿时间： | 1988/6/15 0:00:00 |
AN ANALYSIS OF THE CIRCULATION MECHANISM FOR THE MEDIUM-RANGE ADVANCE AND RETREAT OF THE WEST PACIFIC SUBTROPICAL HIGH |
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| Yu Shihua and Pan Chunsheng.AN ANALYSIS OF THE CIRCULATION MECHANISM FOR THE MEDIUM-RANGE ADVANCE AND RETREAT OF THE WEST PACIFIC SUBTROPICAL HIGH[J].Journal of Tropical Meteorology,1989,0(3):220-226. |
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| Authors: | Yu Shihua and Pan Chunsheng |
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| Institution: | Air Force Institute of Meteorolugy |
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| Abstract: | 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. |
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