摘要
利用NCEP/NCAR1958—1999年5~6月各标准等压面层网格点资料,采用合成法和对比分析等方法,对初夏青藏高原季风和东亚季风环流异常进行了分析。结果表明:四川盆地初夏干旱的季风环流特征是高原季风偏弱,高原季风低压偏西,我国东部地区东亚季风偏弱,东亚季风槽偏南;而多雨年则反之。四川盆地初夏干旱年,极涡向亚洲大陆发展,强度偏强,东亚大槽偏强且稳定;而多雨的年份,极涡萎缩在极地区域,强度偏弱,东亚大槽偏弱。
By using NCEP/NCAR data from May to June 1958—1999, compositing and comparing methods, the anomaly circulations of QinghaiXizang Plateau monsoon and East Asian monsoon are analyzed. The results are as follows: The characteristics of Plateau monsoon and East Asian monsoon for drought and wet years in early summer are different. The Plateau monsoon was weak /strong in drought/wet years and its low pressure was far westward/eastward. East Asian monsoon in the east part of China was also weak /strong and its trough was far southward/northward. Polar vortex developed/shrank towards south/north in drought and wet years in Sichuan basin and deep trough of East Asia was strong/weak.
出处
《高原气象》
CSCD
北大核心
2003年第B10期1-7,共7页
Plateau Meteorology
基金
国家自然科学基金项目(40375031)
中国气象局成都高原气象研究所高原气象开放实验室基金
中国气象局"九五"青年气象科学基金资助
关键词
高原季风
东亚季风
初夏
旱涝
Plateau monsoon
East Asian monsoon
Early summer
Dryness and wetness