| 青藏高原500hpa高压的活动与东亚大型天气系统的演变 |
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| 引用本文： | 段廷阳,邱莎.青藏高原500hpa高压的活动与东亚大型天气系统的演变[J].成都信息工程学院学报,1991(2). |
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| 作者姓名： | 段廷阳 邱莎 |
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| 作者单位： | 成都气象学院气象系
(段廷阳)，湖南省常德气象局(邱莎) |
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| 摘 要： | 本文着重分析了青藏高原500hpa高压因伊朗高压脊东伸、分裂产生过程中和东移过程中,西风带波动、印度季风低压以及100hpa层流型的一系列变化,从而说明青藏高原500hpa高压产生和东移的环流背景。
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| 关 键 词： | 气象学 高原 天气分析 500hpa高压 印度季风低压 伊朗副热带高压脊 |
THE ACTIVITIES OF THE HIGH PRESSURS AT 500hpa LEVEL OVER THE TIBETAN PLATEAU AND THE EVOLUTION OF THE LARGE-SCALE SYNOPTIC SYSTEM OVER EAST ASIA |
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| Dam Tingyang.THE ACTIVITIES OF THE HIGH PRESSURS AT 500hpa LEVEL OVER THE TIBETAN PLATEAU AND THE EVOLUTION OF THE LARGE-SCALE SYNOPTIC SYSTEM OVER EAST ASIA[J].Journal of Chengdu University of Information Technology,1991(2). |
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| Authors: | Dam Tingyang |
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| Abstract: | In this paper,a series of variations of the westerly wave ,the Indian monsoon depression and the flow pattern at 100hpa level in the course of translation and out-growth because of breakaway from the Iranian subtropical ridge of the high pressure at 500hpa level over the Tibetan Plateau are studied and the circulation background is revealed. |
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| Keywords: | Meteorology Plateau Weather analyusis High pressure at 500hpa level Indian monsoon de- pression Iranian subtropical ridge |
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