2006年高原夏季风强弱变化及其与西南地区东部夏季气温和降水的关系

doi:10.11755/j.issn.1006-7639(2015)-04-0555

干旱气象

2006年高原夏季风强弱变化及其与西南地区东部夏季气温和降水的关系

1. 中国气象局成都高原气象研究所，高原与盆地暴雨旱涝灾害四川省重点实验室，四川成都 610072；
2. 交通运输部东海第一救助飞行队，上海 200137

出版日期:2015-08-31 发布日期:2015-08-31
作者简介:齐冬梅（1983-），女，云南人，硕士，主要从事气候变化研究. E-mail:qidongmei1983@163.com
基金资助:
四川省气象局科学技术研究开发课题（川气课题2014-青年-03）、国家自然科学基金青年科学基金（41305082）和中国气象局成都高原气象开放实验室基金课题（BROP201513）共同资助

Intensity Variation of Plateau Summer Monsoon and Its Relation with Summer Temperature and Precipitation in Eastern Part of Southwest China in 2006

1. Chengdu Institute of Plateau Meteorology, China Meteorology Administration, Heavy Rain and Drought-Flood Disasters in Plateau and Basin Key Laboratory of Sichuan Province, Chengdu 610072, China;
2. Donghai No.1 Air Rescue Service, Shanghai 200137, China

Online:2015-08-31 Published:2015-08-31

摘要/Abstract

摘要：

利用2006年西南地区东部37个测站逐日降水量、气温资料和NCEP/NCAR R2再分析日平均资料，通过相关分析和合成分析，研究分析了高原夏季风季节内变化特征，讨论了高原夏季风强弱变化特征及其与西南地区东部夏季气候的关系。结果表明：高原夏季风的变化和西南地区东部夏季气候变化关系密切。当高原夏季风偏强（弱）时，南亚高压、中高纬度环流、西太副高、西风带环流、低层流场以及垂直运动等均有显著变化，进而影响到西南地区东部夏季气候。高原夏季风的季节内变化与青藏高原大气热源呈显著正相关关系，青藏高原热力作用对高原夏季风的异常变化有重要作用。

关键词: 高原季风, 大气环流异常, 高原热源, 高温干旱, 西南地区东部

Abstract:

Based on the daily precipitation and temperature data at 37 meteorological stations in eastern southwest China and NCEP/NCAR R2 reanalysis data in 2006, the variation characteristics of the plateau summer monsoon and its relation with summer climate in eastern southwest China were analyzed and discussed by the correlation analysis and composite analysis. The results showed that the variations of plateau summer monsoon had close connection with summer climate in eastern southwest China in 2006. The variations of plateau summer monsoon intensity were closely related with persistent anomalies of atmospheric circulation in the same period, such as the South Asia High(SAH), atmospheric circulation anomalies in the mid-high latitude, Western Pacific Subtropical High(WPSH), westerly belt circulation, lower-level flow field, vertical movement and so on, and then affected climate change in eastern southwest China in summer of 2006. Furthermore，the correlation between the seasonal change of plateau summer monsoon and the atmospheric heat source over Tibetan plateau in summer of 2006 was obviously positive. The thermal effects of atmosphere over Tibetan Plateau played an important role in anomalous variation of the plateau summer monsoon.

Key words: plateau monsoon, anomalous atmospheric circulation, atmospheric heat source over Tibetan Plateau, high temperature and drought, in eastern southwest China

中图分类号:

P426.616

齐冬梅1，李英1，李跃清1，刘昆鹏2. 2006年高原夏季风强弱变化及其与西南地区东部夏季气温和降水的关系[J]. 干旱气象, DOI: 10.11755/j.issn.1006-7639(2015)-04-0555.

QI Dongmei1, LI Ying1, LI Yueqing1, LIU Kunpeng2. Intensity Variation of Plateau Summer Monsoon and Its Relation with Summer Temperature and Precipitation in Eastern Part of Southwest China in 2006[J]. Journal of Arid Meteorology, DOI: 10.11755/j.issn.1006-7639(2015)-04-0555.

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2006年高原夏季风强弱变化及其与西南地区东部夏季气温和降水的关系

Intensity Variation of Plateau Summer Monsoon and Its Relation with Summer Temperature and Precipitation in Eastern Part of Southwest China in 2006

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