THE INTERDECADAL VARIABILITY OF ADVANCE AND RETREAT OF EAST ASIAN SUMMER MONSOON AND THEIR EFFECT ON THE REGIONAL RAINFALL OVER CHINA
Lu Xin-yan1; Zhang Xiu-zhi2; Chen Jin-nian3
刊名JOURNAL OF TROPICAL METEOROLOGY
2013-12-01
卷号19期号:4页码:340-348
关键词EASM index front of EASM movement of EASM interdecadal variability rainfall over China
ISSN号1006-8775
通讯作者Lu, XY
中文摘要The daily precipitation data of 740 stations in China (1958-2001) and the daily upper air data of European Centre for Medium-Range Weather Forecasts reanalysis dataset (1958-2001) are used to define an East Asian summer monsoon (EASM) index based on dynamic and thermal factors. The index is used to represent the front (or leading edge) of EASM to describe and characterize the advance and retreat of EASM objectively. During 1958-2001, the EASM movement underwent three interdecadal abrupt shifts in 1965, 1980 and 1994, respectively. During 1958-1964, the front primarily concentrated in South China and North China, while it stayed at the mid- and lower-Yangtze River for a short period. During 1965-1979, the front was located in South China and the lower reach of Yellow River for a long time. During 1980-1993, the time in which the front of EASM stayed at the mid- and lower-Yangtze River was much longer, but it settled in North China for just a short time. During 1994-2001, the front generally concentrated in the south of the mid- and lower-Yangtze River. The three interdecadal shifts of EASM directly resulted in rainfall anomalies, as well as frequent disasters of flood and drought in East China.
英文摘要The daily precipitation data of 740 stations in China (1958-2001) and the daily upper air data of European Centre for Medium-Range Weather Forecasts reanalysis dataset (1958-2001) are used to define an East Asian summer monsoon (EASM) index based on dynamic and thermal factors. The index is used to represent the front (or leading edge) of EASM to describe and characterize the advance and retreat of EASM objectively. During 1958-2001, the EASM movement underwent three interdecadal abrupt shifts in 1965, 1980 and 1994, respectively. During 1958-1964, the front primarily concentrated in South China and North China, while it stayed at the mid- and lower-Yangtze River for a short period. During 1965-1979, the front was located in South China and the lower reach of Yellow River for a long time. During 1980-1993, the time in which the front of EASM stayed at the mid- and lower-Yangtze River was much longer, but it settled in North China for just a short time. During 1994-2001, the front generally concentrated in the south of the mid- and lower-Yangtze River. The three interdecadal shifts of EASM directly resulted in rainfall anomalies, as well as frequent disasters of flood and drought in East China.
学科主题Meteorology & Atmospheric Sciences
WOS标题词Science & Technology ; Physical Sciences
类目[WOS]Meteorology & Atmospheric Sciences
研究领域[WOS]Meteorology & Atmospheric Sciences
收录类别SCI
语种英语
WOS记录号WOS:000328590100004
公开日期2014-07-17
内容类型期刊论文
源URL[http://ir.qdio.ac.cn/handle/337002/16440]  
专题海洋研究所_海洋环流与波动重点实验室
作者单位1.Natl Meteorol Ctr, Beijing 100081, Peoples R China
2.Natl Climate Ctr, Beijing 100081, Peoples R China
3.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China
推荐引用方式
GB/T 7714
Lu Xin-yan,Zhang Xiu-zhi,Chen Jin-nian. THE INTERDECADAL VARIABILITY OF ADVANCE AND RETREAT OF EAST ASIAN SUMMER MONSOON AND THEIR EFFECT ON THE REGIONAL RAINFALL OVER CHINA[J]. JOURNAL OF TROPICAL METEOROLOGY,2013,19(4):340-348.
APA Lu Xin-yan,Zhang Xiu-zhi,&Chen Jin-nian.(2013).THE INTERDECADAL VARIABILITY OF ADVANCE AND RETREAT OF EAST ASIAN SUMMER MONSOON AND THEIR EFFECT ON THE REGIONAL RAINFALL OVER CHINA.JOURNAL OF TROPICAL METEOROLOGY,19(4),340-348.
MLA Lu Xin-yan,et al."THE INTERDECADAL VARIABILITY OF ADVANCE AND RETREAT OF EAST ASIAN SUMMER MONSOON AND THEIR EFFECT ON THE REGIONAL RAINFALL OVER CHINA".JOURNAL OF TROPICAL METEOROLOGY 19.4(2013):340-348.
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