Precipitation variations of Longxi, northeast margin of Tibetan Plateau since AD 960 and their relationship with solar activity

	Precipitation variations of Longxi, northeast margin of Tibetan Plateau since AD 960 and their relationship with solar activity
	Tan, Liangcheng 1,3; Cai, Yanjun 1; Yi, Liang 2,3; An, Zhisheng 1; Ai, Li 1,3
发表期刊	CLIMATE OF THE PAST
ISSN	1814-9324
	2008
卷号	4 期号:1 页码:19-28
关键词	Climate-change Peat Cellulose Asian Monsoon Drought Frequency Atlantic Climate Holocene Climate Tree-rings China Sea Variability Record
产权排序	[Tan, Liangcheng; Cai, Yanjun; An, Zhisheng; Ai, Li] Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China; [Yi, Liang] Chinese Acad Sci, Yantai Inst Coastal Zone Res Sustainable Dev, Yantai 264003, Peoples R China; [Tan, Liangcheng; Yi, Liang; Ai, Li] Chinese Acad Sci, Grad Sch, Beijing 100039, Peoples R China
英文摘要	The precipitation variations of Longxi area, northeast margin of the Tibetan Plateau since AD 960 are reconstructed from Chinese historical documentary records. These records show that since AD 960, the precipitation of Longxi decreased and reached the lowest level at the end of the 17th and the 18th centuries. After this period, the precipitation gradually increased. The three short wet periods of Longxi in the last millennium were: from the end of the 10th century to the early years of the 11th century, from the end of the 12th century to the early years of the 13th century and during the first half of the 20th century. The precipitation variations coincide well with variations of the Northern Hemisphere temperature and the atmospheric 14C concentration, as well as the averaged 10Be concentration and the reconstructed solar modulation record which show that solar activity may be an important driving force of the precipitation variations of Longxi on multi-decadal to centennial scales during the last millennium. Solar activity controls the motion of the north edge of the Asian summer monsoon by affecting the Asia summer monsoon intensity, the East Asian winter monsoon intensity and the locations of westerlies, thus further dominating precipitation variations of Longxi. Synchronous variations of Longxi precipitation and Northern Hemisphere temperature may also be ascribed to the same control of solar activity.; The precipitation variations of Longxi area, northeast margin of the Tibetan Plateau since AD 960 are reconstructed from Chinese historical documentary records. These records show that since AD 960, the precipitation of Longxi decreased and reached the lowest level at the end of the 17th and the 18th centuries. After this period, the precipitation gradually increased. The three short wet periods of Longxi in the last millennium were: from the end of the 10th century to the early years of the 11th century, from the end of the 12th century to the early years of the 13th century and during the first half of the 20th century. The precipitation variations coincide well with variations of the Northern Hemisphere temperature and the atmospheric (14)C concentration, as well as the averaged (10)Be concentration and the reconstructed solar modulation record which show that solar activity may be an important driving force of the precipitation variations of Longxi on multi-decadal to centennial scales during the last millennium. Solar activity controls the motion of the north edge of the Asian summer monsoon by affecting the Asia summer monsoon intensity, the East Asian winter monsoon intensity and the locations of westerlies, thus further dominating precipitation variations of Longxi. Synchronous variations of Longxi precipitation and Northern Hemisphere temperature may also be ascribed to the same control of solar activity.
文章类型	Article
收录类别	SCI
语种	英语
关键词[WOS]	CLIMATE-CHANGE ; PEAT CELLULOSE ; ASIAN MONSOON ; DROUGHT FREQUENCY ; ATLANTIC CLIMATE ; HOLOCENE CLIMATE ; TREE-RINGS ; CHINA SEA ; VARIABILITY ; RECORD
研究领域[WOS]	Geology ; Meteorology & Atmospheric Sciences
WOS记录号	WOS:000253673000003
引用统计	被引频次：81[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.yic.ac.cn/handle/133337/4429
专题	中国科学院烟台海岸带研究所知识产出
作者单位	1.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China 2.Chinese Acad Sci, Yantai Inst Coastal Zone Res Sustainable Dev, Yantai 264003, Peoples R China 3.Chinese Acad Sci, Grad Sch, Beijing 100039, Peoples R China
推荐引用方式 GB/T 7714	Tan, Liangcheng,Cai, Yanjun,Yi, Liang,et al. Precipitation variations of Longxi, northeast margin of Tibetan Plateau since AD 960 and their relationship with solar activity[J]. CLIMATE OF THE PAST,2008,4(1):19-28.
APA	Tan, Liangcheng,Cai, Yanjun,Yi, Liang,An, Zhisheng,&Ai, Li.(2008).Precipitation variations of Longxi, northeast margin of Tibetan Plateau since AD 960 and their relationship with solar activity.CLIMATE OF THE PAST,4(1),19-28.
MLA	Tan, Liangcheng,et al."Precipitation variations of Longxi, northeast margin of Tibetan Plateau since AD 960 and their relationship with solar activity".CLIMATE OF THE PAST 4.1(2008):19-28.

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