J4 ›› 2007, Vol. 25 ›› Issue (4): 74-79.

• 综述 • 上一篇    下一篇

高原季风研究主要进展及其科学意义

齐冬梅1, 2 ,李跃清2   

  1. 1. 中国气象局气象科学研究院,北京 100081; 2. 中国气象局成都高原气象研究所,四川 成都 610071
  • 收稿日期:2007-10-30 修回日期:2007-11-22 出版日期:2007-12-31 发布日期:2007-12-31
  • 作者简介:齐冬梅(1983 - ) ,女,汉,云南人,硕士研究生,主要从事高原气候研究. E - mail: qidongmei1983@163. com
  • 基金资助:

    国家重点基础研究发展计划(2003CB415201 - 6) ,中国气象局气候变化专项(CCSF2007 - 23) ,青藏高原及临近地区水循环中大气过程的气候特征研究(BROP200702) ,江苏省气象灾害重点基金项目(KLME050210)共同资助

The Major Progress of the PlateauM on soon Study and its Scien tif ic Sign if icance

Q IDongmei , L I Yueqing   

  1. 1. Chinese Academ y ofM eteorological Sciences, CMA, B eijing 100081, China;2. Institute of Plateau M eteorology, CMA, Chengdu 610071, China
  • Received:2007-10-30 Revised:2007-11-22 Online:2007-12-31 Published:2007-12-31

摘要:

季风是气象界的“永恒”课题,已有数百年的研究历史。亚洲季风系统中存在着3个相对独立的子系统:南亚季风、东亚季风和高原季风。简要总结了国内外关于高原季风的若干研究进展,对比分析了各阶段高原季风研究的特点。同时指出今后应进一步丰富高原季风指数定义,并对高原季风变化的物理成因等方面进行深入研究

关键词: 高原季风, 高原气候, 季风指数

Abstract:

Monsoon is a popular subject in the field of meteorology and has been studied for centuries. Analysis shows that the Asian monsoon system can be categorized into three relatively independent sub - systems, including South Asian monsoon, East Asian monsoon, and p lateau monsoon. This paper summarizes the study achievements on p lateau monsoon, and it analyzes the characteristics of the p lateau monsoon at different research stages. In addition, it points out that the future study should be focused on a better definition about p lateau monsoon index and the physical causes of the p lateau monsoon change.

Key words:  plateau monsoon, p lateau climate, plateau monsoon index

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