中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Temperature changes on the Tibetan Plateau during the past 600 years inferred from ice cores and tree rings

文献类型:期刊论文

作者Yang, Bao1,2,3; Braeuning, Achim3; Liu, Jingjing1; Davis, Mary E.4; Yajun, Shao1
刊名GLOBAL AND PLANETARY CHANGE
出版日期2009-10-01
卷号69期号:1-2页码:71-78
关键词Puruogangri ice cap climate change ice cores tree rings Tibetan Plateau
ISSN号0921-8181
DOI10.1016/j.gloplacha.2009.07.008
通讯作者Yang, Bao(yangbao@lzb.ac.cn)
英文摘要The climatological signal of delta O-18 variations preserved in ice cores recovered from Puruogangri ice field in the central Tibetan Plateau (TP) was calibrated with regional meteorological data for the past 50 years. For the period AD 1860-2000, 5-yearly averaged ice core delta O-18 and a summer temperature reconstruction derived from pollen data from the same ice core were compared. The statistical results provide compelling evidence that Puruogangri ice core delta O-18 variations represent summer temperature changes for the central TP, and hence regional temperature history during the past 600 years was revealed. A comparison of Puruogangri ice core delta O-18 with several other temperature reconstructions shows that broad-scale climate anomalies since the Little Ice Age occurred synchronously across the eastern and southern TP. and the Himalayas. Common cold periods were identified in the 15th century, 1625-1645 AD, 1660-1700 AD, 1725-1775 AD, 1795-1830 AD. 1850-1870 AD, 1890-1920 AD, 1940-1950 AD, and 1975-1985 AD. The period 1725-1775 AD was one of the most prolonged cool periods during the past 400 years and corresponded to maximum Little Ice Age glacier advance of monsoonal temperate glaciers of the TP. (C) 2009 Elsevier B.V. All rights reserved.
收录类别SCI
WOS关键词CENTRAL HENGDUAN MOUNTAINS ; LAST MILLENNIUM ; QAIDAM BASIN ; CENTRAL-ASIA ; PRECIPITATION VARIATION ; ENVIRONMENTAL-CHANGES ; STABLE-ISOTOPES ; NORTHWEST CHINA ; SUMMER MONSOON ; CLIMATE-CHANGE
WOS研究方向Physical Geography ; Geology
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
语种英语
WOS记录号WOS:000271370100007
出版者ELSEVIER SCIENCE BV
URI标识http://www.irgrid.ac.cn/handle/1471x/2556269
专题寒区旱区环境与工程研究所
通讯作者Yang, Bao
作者单位1.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Key Lab Desert & Desertificat, Lanzhou, Gansu, Peoples R China
2.Lanzhou Univ, Coll Earth & Environm Sci, MOE Key Lab W Chinas Environm Syst, Lanzhou 730000, Gansu, Peoples R China
3.Univ Erlangen Nurnberg, Inst Geog, D-91054 Erlangen, Germany
4.Ohio State Univ, Byrd Polar Res Ctr, Columbus, OH 43210 USA
推荐引用方式
GB/T 7714
Yang, Bao,Braeuning, Achim,Liu, Jingjing,et al. Temperature changes on the Tibetan Plateau during the past 600 years inferred from ice cores and tree rings[J]. GLOBAL AND PLANETARY CHANGE,2009,69(1-2):71-78.
APA Yang, Bao,Braeuning, Achim,Liu, Jingjing,Davis, Mary E.,&Yajun, Shao.(2009).Temperature changes on the Tibetan Plateau during the past 600 years inferred from ice cores and tree rings.GLOBAL AND PLANETARY CHANGE,69(1-2),71-78.
MLA Yang, Bao,et al."Temperature changes on the Tibetan Plateau during the past 600 years inferred from ice cores and tree rings".GLOBAL AND PLANETARY CHANGE 69.1-2(2009):71-78.

入库方式: iSwitch采集

来源:寒区旱区环境与工程研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。