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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