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。
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.
出处
《成都信息工程学院学报》
1991年第2期10-15,共6页
Journal of Chengdu University of Information Technology
基金
国家气象局气象科学基金
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
Meteorology
Plateau
Weather analyusis
High pressure at 500hpa level
Indian monsoon de- pression
Iranian subtropical ridge.
