Early summer temperature reconstruction in the eastern Tibetan plateau since ad 1440 using tree-ring width of Sabina tibetica

被引：38

作者：

Zhu, Hai-Feng ^{[1
,2
]}

Shao, Xue-Mei ^{[2
]}

Yin, Zhi-Yong ^{[3
]}

Huang, Lei ^{[4
]}

机构：

[1] Chinese Acad Sci, Key Lab Tibetan Environm Changes & Land Surface P, Inst Tibetan Plateau Res, Beijing 100085, Peoples R China

[2] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China

[3] Univ San Diego, Dept Marine Sci & Environm Studies, San Diego, CA 92110 USA

[4] Natl Climate Ctr, Beijing 100081, Peoples R China

来源：

THEORETICAL AND APPLIED CLIMATOLOGY | 2011年 / 106卷 / 1-2期

基金：

中国国家自然科学基金;

关键词：

PRECIPITATION VARIATION; QINGHAI PROVINCE; MEAN TEMPERATURE; QILIAN MOUNTAINS; WESTERN HIMALAYA; MONSOON; VARIABILITY; HISTORY; RECORD; ONSET;

D O I：

10.1007/s00704-011-0419-7

中图分类号：

P4 [大气科学（气象学）];

学科分类号：

0706 ; 070601 ;

摘要：

Long climate records are scarce on the Tibetan Plateau for understanding the climate variability on long-term context. Here we presented an early summer (May-June) temperature reconstruction since ad 1440 for Qamdo area using tree rings of Sabina tibetica. The reconstruction accounted for 64% of the variance in the instrumental record. It showed warm periods during 1501-1514, 1528-1538, 1598-1609, 1624-1636, 1650-1668, 1695-1705, 1752-1762, 1794-1804, 1878-1890, 1909-1921, 1938-1949, and 1979-1991. Cool early summer occurred during 1440-1454, 1482-1500, 1515-1527, 1576-1597, 1610-1621, 1669-1679, 1706-1716, 1782-1793, 1863-1873, 1894-1908, and 1922-1937. Comparison with other proxy or meteorological records suggested that there is obvious spatial variability in the May-June temperature variations along the eastern margin of the Tibetan Plateau.

引用

页码：45 / 53

页数：9

共 48 条

[21] Dendrochronological potential of the alpine shrub Rhododendron nivale on the south-eastern Tibetan Plateau [J].

Liang, Eryuan ;

Eckstein, Dieter .

ANNALS OF BOTANY, 2009, 104 (04) :665-670

[22]

Liu X, 2007, ARCT ANTARCT ALP RES, V39, P651, DOI 10.1657/1523-0430(07-506)[LIU-X]2.0.CO

[23]

[24] Precipitation variation in the northeastern Tibetan Plateau recorded by the tree rings since 850 AD and its relevance to the Northern Hemisphere temperature [J].

Liu Yu ;

An Zhisheng ;

Ma Haizhou ;

Cai Qiufang ;

Liu Zhengyu ;

Kutzbach, John K. ;

Shi Jiangfeng ;

Song Huiming ;

Sun Junyan ;

Yi Liang ;

Li Qiang ;

Yang Yinke ;

Wang Lei .

SCIENCE IN CHINA SERIES D-EARTH SCIENCES, 2006, 49 (04) :408-420

[25] Robust estimation of background noise and signal detection in climatic time series [J].

Mann, ME ;

Lees, JM .

CLIMATIC CHANGE, 1996, 33 (03) :409-445

[26]

MICHAELSEN J, 1987, J CLIM APPL METEOROL, V26, P1589, DOI 10.1175/1520-0450(1987)026<1589:CVISCF>2.0.CO

[27]

[28] An improved method of constructing a database of monthly climate observations and associated high-resolution grids [J].

Mitchell, TD ;

Jones, PD .

INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2005, 25 (06) :693-712

[29] Climatic implications of a 3585-year tree-ring width chronology from the northeastern Qinghai-Tibetan Plateau [J].

Shao, X. ;

Xu, Y. ;

Yin, Z-Y ;

Liang, E. ;

Zhu, H. ;

Wang, S. .

QUATERNARY SCIENCE REVIEWS, 2010, 29 (17-18) :2111-2122

[30] Reconstruction of precipitation variation from tree rings in recent 1000 years in Delingha, Qinghai [J].

Shao, XM ;

Huang, L ;

Liu, HB ;

Liang, EY ;

Fang, XQ ;

Wang, LL .

SCIENCE IN CHINA SERIES D-EARTH SCIENCES, 2005, 48 (07) :939-949

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