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Onset of East Asian subtropical summer monsoon and rainy season in China

查看全文 作  者:ZHU [1]CongWen;ZHOU [1]XiuJi;ZHAO [2]Ping;CHEN [1]LongXun;HE [3]JinHai 高影响力作者 机构地区:[1]Chinese Academy of Meteorological Sciences, Beijing 100081, China;[2]National Information Center, Chinese Meteorological Administration, Beijing 100081, China;[3]Nanjing University oflnformation Science & Technology, Nanjing 210044, China高影响力机构 出  处:《Science China Earth Sciences》索引2011年第54卷第12期,共9页高影响力期刊 基  金:supported by the National Natural Science Foundation of China (Grant Nos. 40921003 and 90711003);the Program of the Chinese Academy of Meteorological Sciences (Grant Nos. 2010Z003 and GYHY 200706005) 摘  要:Here we use harmonic analyses to examine seasonal variations of China land rainfall, low-level winds, and atmospheric heating over East Asia during spring to summer and the associated subtropical summer monsoon activities. Our results indicate that the South China spring rainfall (SCSR) in March is the prophase of East Asian sub-tropical summer monsoon (EASSM), and the onset of EASSM and China summer rainy season starts in early April, characterized by the enhanced rainfall in South China and the seasonal reverse of zonal land-sea thermal contrast in sub-tropical East Asia. The EASSM onset is earlier than that of South China Sea summer monsoon, and it is active in east of 100?E and north of 20?N. Our analyses suggest that the subsequent heating appears over India-China Peninsula in March and South China in April and causes the low-level atmospheric warming and the zonal land-sea thermal contrast seasonal reverse in East Asian subtropics. The atmospheric heating over South China is the main force to drive the southwesterly winds, updrafts and strengthen the summer precipitation in South China. 关 键 词:中国南方 夏季季风 副热带 东亚 发病 雨季 季节性变化 夏季风活动
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