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Holocene Abrupt Climate Shifts and Mid-Holocene Drought Intervals Recorded in Barkol Lake of Northern Xinjiang of China

XUE Jibin,  ZHONG Wei,  ZHAO Yinjuan,  PENG Xiaoying

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文章导航 > Chinese Geographical Science  > 2008 >  18(1): 54-61
XUE Jibin, ZHONG Wei, ZHAO Yinjuan, PENG Xiaoying. Holocene Abrupt Climate Shifts and Mid-Holocene Drought Intervals Recorded in Barkol Lake of Northern Xinjiang of China[J]. 中国地理科学, 2008, 18(1): 54-61. doi: 10.1007/s11769-008-0054-0
引用本文: XUE Jibin, ZHONG Wei, ZHAO Yinjuan, PENG Xiaoying. Holocene Abrupt Climate Shifts and Mid-Holocene Drought Intervals Recorded in Barkol Lake of Northern Xinjiang of China[J]. 中国地理科学, 2008, 18(1): 54-61. doi: 10.1007/s11769-008-0054-0
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XUE Jibin, ZHONG Wei, ZHAO Yinjuan, PENG Xiaoying. Holocene Abrupt Climate Shifts and Mid-Holocene Drought Intervals Recorded in Barkol Lake of Northern Xinjiang of China[J]. Chinese Geographical Science, 2008, 18(1): 54-61. doi: 10.1007/s11769-008-0054-0
Citation: XUE Jibin, ZHONG Wei, ZHAO Yinjuan, PENG Xiaoying. Holocene Abrupt Climate Shifts and Mid-Holocene Drought Intervals Recorded in Barkol Lake of Northern Xinjiang of China[J]. Chinese Geographical Science, 2008, 18(1): 54-61. doi: 10.1007/s11769-008-0054-0
shu

Holocene Abrupt Climate Shifts and Mid-Holocene Drought Intervals Recorded in Barkol Lake of Northern Xinjiang of China

doi: 10.1007/s11769-008-0054-0
  • 1.

    School of Geography Science, South China Normal University, Guangzhou 510631, China;

  • 2.

    National Laboratory of Western China's Environmental Systems, Lanzhou University, Lanzhou 730000, China

基金项目: Under the auspices of National Natural Science Foundation of China (No. 49761007);Open Foundation of National Laboratory of Western China's Environmental Systems,Lanzhou University
详细信息
    通讯作者:

    ZHONG Wei. E-mail: DL06@scnu.edu.cn

Holocene Abrupt Climate Shifts and Mid-Holocene Drought Intervals Recorded in Barkol Lake of Northern Xinjiang of China

  • 1.

    School of Geography Science, South China Normal University, Guangzhou 510631, China;

  • 2.

    National Laboratory of Western China's Environmental Systems, Lanzhou University, Lanzhou 730000, China

Funds: Under the auspices of National Natural Science Foundation of China (No. 49761007);Open Foundation of National Laboratory of Western China's Environmental Systems,Lanzhou University

  • 摘要: Study results in this paper have indicated that the Holocene climate in Xinjiang,Northwestern China has been alternating between wet and dry conditions,and was punctuated with a series of abrupt climate shifts.A sediment core taken from Barkol Lake in the northern Xinjiang of Northwest China was analyzed at 1cm interval for grain-size distribution.Abrupt climate shifts revealed by the grain-size proxy occurred at ca 1.4,3.0,4.3,5.6,8.0 cal kyr B.P.,which were well correlated to both the abrupt shifts recorded in the North Atlantic Ocean(NAO)and the Holocene sea surface temperature(SST)cooling events in the Arabian Ocean.The correlation indicated that the climatic changes in the extreme arid Northwest China were associated with the NAO,probably via the North Atlantic Oscillation-affected westerly winds.The strength and position of westerly winds probably modulated the Siberian-Mongolian high-pressure system(winter monsoon),and played an important role in climate change of Northwest China.Moreover,an evident drought interval during the middle Holocene was also revealed by grain-size proxy.
    Abstract: Study results in this paper have indicated that the Holocene climate in Xinjiang,Northwestern China has been alternating between wet and dry conditions,and was punctuated with a series of abrupt climate shifts.A sediment core taken from Barkol Lake in the northern Xinjiang of Northwest China was analyzed at 1cm interval for grain-size distribution.Abrupt climate shifts revealed by the grain-size proxy occurred at ca 1.4,3.0,4.3,5.6,8.0 cal kyr B.P.,which were well correlated to both the abrupt shifts recorded in the North Atlantic Ocean(NAO)and the Holocene sea surface temperature(SST)cooling events in the Arabian Ocean.The correlation indicated that the climatic changes in the extreme arid Northwest China were associated with the NAO,probably via the North Atlantic Oscillation-affected westerly winds.The strength and position of westerly winds probably modulated the Siberian-Mongolian high-pressure system(winter monsoon),and played an important role in climate change of Northwest China.Moreover,an evident drought interval during the middle Holocene was also revealed by grain-size proxy.
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  • 收稿日期:  2007-07-02
  • 修回日期:  2007-12-21
  • 刊出日期:  2008-03-20

Holocene Abrupt Climate Shifts and Mid-Holocene Drought Intervals Recorded in Barkol Lake of Northern Xinjiang of China

doi: 10.1007/s11769-008-0054-0
  • 1. School of Geography Science, South China Normal University, Guangzhou 510631, China;
  • 2. National Laboratory of Western China's Environmental Systems, Lanzhou University, Lanzhou 730000, China
    • 基金项目:  Under the auspices of National Natural Science Foundation of China (No. 49761007);Open Foundation of National Laboratory of Western China's Environmental Systems,Lanzhou University
    通讯作者: ZHONG Wei. E-mail: DL06@scnu.edu.cn
  • 收稿日期: 2007-07-02
  • 修回日期: 2007-12-21
  • 刊出日期: 2008-03-20

摘要: Study results in this paper have indicated that the Holocene climate in Xinjiang,Northwestern China has been alternating between wet and dry conditions,and was punctuated with a series of abrupt climate shifts.A sediment core taken from Barkol Lake in the northern Xinjiang of Northwest China was analyzed at 1cm interval for grain-size distribution.Abrupt climate shifts revealed by the grain-size proxy occurred at ca 1.4,3.0,4.3,5.6,8.0 cal kyr B.P.,which were well correlated to both the abrupt shifts recorded in the North Atlantic Ocean(NAO)and the Holocene sea surface temperature(SST)cooling events in the Arabian Ocean.The correlation indicated that the climatic changes in the extreme arid Northwest China were associated with the NAO,probably via the North Atlantic Oscillation-affected westerly winds.The strength and position of westerly winds probably modulated the Siberian-Mongolian high-pressure system(winter monsoon),and played an important role in climate change of Northwest China.Moreover,an evident drought interval during the middle Holocene was also revealed by grain-size proxy.

English Abstract

XUE Jibin, ZHONG Wei, ZHAO Yinjuan, PENG Xiaoying. Holocene Abrupt Climate Shifts and Mid-Holocene Drought Intervals Recorded in Barkol Lake of Northern Xinjiang of China[J]. 中国地理科学, 2008, 18(1): 54-61. doi: 10.1007/s11769-008-0054-0
引用本文: XUE Jibin, ZHONG Wei, ZHAO Yinjuan, PENG Xiaoying. Holocene Abrupt Climate Shifts and Mid-Holocene Drought Intervals Recorded in Barkol Lake of Northern Xinjiang of China[J]. 中国地理科学, 2008, 18(1): 54-61. doi: 10.1007/s11769-008-0054-0
shu
XUE Jibin, ZHONG Wei, ZHAO Yinjuan, PENG Xiaoying. Holocene Abrupt Climate Shifts and Mid-Holocene Drought Intervals Recorded in Barkol Lake of Northern Xinjiang of China[J]. Chinese Geographical Science, 2008, 18(1): 54-61. doi: 10.1007/s11769-008-0054-0
Citation: XUE Jibin, ZHONG Wei, ZHAO Yinjuan, PENG Xiaoying. Holocene Abrupt Climate Shifts and Mid-Holocene Drought Intervals Recorded in Barkol Lake of Northern Xinjiang of China[J]. Chinese Geographical Science, 2008, 18(1): 54-61. doi: 10.1007/s11769-008-0054-0
shu

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