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CLIMATIC VARIATIONS IN CHINA OVER THE LAST 2000 YEARS

YANG Bao,  SHI Ya-feng,  LI Heng-peng

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文章导航 > Chinese Geographical Science  > 2001 >  11(2): 97-103
YANG Bao, SHI Ya-feng, LI Heng-peng. CLIMATIC VARIATIONS IN CHINA OVER THE LAST 2000 YEARS[J]. 中国地理科学, 2001, 11(2): 97-103.
引用本文: YANG Bao, SHI Ya-feng, LI Heng-peng. CLIMATIC VARIATIONS IN CHINA OVER THE LAST 2000 YEARS[J]. 中国地理科学, 2001, 11(2): 97-103.
shu
YANG Bao, SHI Ya-feng, LI Heng-peng. CLIMATIC VARIATIONS IN CHINA OVER THE LAST 2000 YEARS[J]. Chinese Geographical Science, 2001, 11(2): 97-103.
Citation: YANG Bao, SHI Ya-feng, LI Heng-peng. CLIMATIC VARIATIONS IN CHINA OVER THE LAST 2000 YEARS[J]. Chinese Geographical Science, 2001, 11(2): 97-103.
shu

CLIMATIC VARIATIONS IN CHINA OVER THE LAST 2000 YEARS

  • 1.

    Cold and And Regions Environmental and Engineering Research Institute, the Chinese Academy of Sciences, Lanzhou 730000, P. R. China;

  • 2.

    Institute of Geography and Limnology, the Chinese Academy of Sciences, Nanjing 210008, P. R. China

基金项目: Under the auspices of the KZCX2-304 and KI 951-A1-202-04 Project of the Chinese Academy of Sciences.
详细信息
    作者简介:

    YANG Bao(1971- ), male, a native of Shanxi, post-doctor. His research interest includes wind-blown sand environment and global change.

  • 中图分类号: P532

CLIMATIC VARIATIONS IN CHINA OVER THE LAST 2000 YEARS

  • 1.

    Cold and And Regions Environmental and Engineering Research Institute, the Chinese Academy of Sciences, Lanzhou 730000, P. R. China;

  • 2.

    Institute of Geography and Limnology, the Chinese Academy of Sciences, Nanjing 210008, P. R. China

Funds: Under the auspices of the KZCX2-304 and KI 951-A1-202-04 Project of the Chinese Academy of Sciences.

  • 摘要: A compilation of paleoclimate records from ice core, tree-rings, lake sediments and historical documents provides a view of temperature change in China over the recent 2000 years. For all-China temperature reconstruction, six sub-stages are identified for the last two millennia. Around AD 0-240, AD 800-1100, AD 1320-1400 and the period from AD 1880 on were warm while around AD 240-800, AD 1100-1320, AD 1400-1880 were cold. Also, temperature varied from region to region in each of the warm or cold periods. The Eastern Han warm period (0-AD 240), the cold period covering the span of Wei, Jin, and the Southern and Northern Dynasties, the MWP (AD 800-1100) and succeeding LIA occurred in eastern China and the Qilian Mountains. Only the fint two climatic events were recorded in Guliya ice core while the so-called MWP and LIA was far weaker. Also, the warming between AD 800 and 1100 didn't occur in the south of Xizang (Tibet) Plateau. Instead, the southern Xizang Plateau experienced warming in AD 1150-1400. The aggregated China temperature agrees well with North-hemisphere temperature in the past millennia, indicating close relationship of temperature changes between China and North-hemisphere.
    Abstract: A compilation of paleoclimate records from ice core, tree-rings, lake sediments and historical documents provides a view of temperature change in China over the recent 2000 years. For all-China temperature reconstruction, six sub-stages are identified for the last two millennia. Around AD 0-240, AD 800-1100, AD 1320-1400 and the period from AD 1880 on were warm while around AD 240-800, AD 1100-1320, AD 1400-1880 were cold. Also, temperature varied from region to region in each of the warm or cold periods. The Eastern Han warm period (0-AD 240), the cold period covering the span of Wei, Jin, and the Southern and Northern Dynasties, the MWP (AD 800-1100) and succeeding LIA occurred in eastern China and the Qilian Mountains. Only the fint two climatic events were recorded in Guliya ice core while the so-called MWP and LIA was far weaker. Also, the warming between AD 800 and 1100 didn't occur in the south of Xizang (Tibet) Plateau. Instead, the southern Xizang Plateau experienced warming in AD 1150-1400. The aggregated China temperature agrees well with North-hemisphere temperature in the past millennia, indicating close relationship of temperature changes between China and North-hemisphere.
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出版历程
  • 收稿日期:  2001-02-13
  • 刊出日期:  2001-06-20

CLIMATIC VARIATIONS IN CHINA OVER THE LAST 2000 YEARS

  • 1. Cold and And Regions Environmental and Engineering Research Institute, the Chinese Academy of Sciences, Lanzhou 730000, P. R. China;
  • 2. Institute of Geography and Limnology, the Chinese Academy of Sciences, Nanjing 210008, P. R. China
    • 基金项目:  Under the auspices of the KZCX2-304 and KI 951-A1-202-04 Project of the Chinese Academy of Sciences.
    作者简介:

    YANG Bao(1971- ), male, a native of Shanxi, post-doctor. His research interest includes wind-blown sand environment and global change.

  • 收稿日期: 2001-02-13
  • 刊出日期: 2001-06-20

  • 中图分类号: P532

摘要: A compilation of paleoclimate records from ice core, tree-rings, lake sediments and historical documents provides a view of temperature change in China over the recent 2000 years. For all-China temperature reconstruction, six sub-stages are identified for the last two millennia. Around AD 0-240, AD 800-1100, AD 1320-1400 and the period from AD 1880 on were warm while around AD 240-800, AD 1100-1320, AD 1400-1880 were cold. Also, temperature varied from region to region in each of the warm or cold periods. The Eastern Han warm period (0-AD 240), the cold period covering the span of Wei, Jin, and the Southern and Northern Dynasties, the MWP (AD 800-1100) and succeeding LIA occurred in eastern China and the Qilian Mountains. Only the fint two climatic events were recorded in Guliya ice core while the so-called MWP and LIA was far weaker. Also, the warming between AD 800 and 1100 didn't occur in the south of Xizang (Tibet) Plateau. Instead, the southern Xizang Plateau experienced warming in AD 1150-1400. The aggregated China temperature agrees well with North-hemisphere temperature in the past millennia, indicating close relationship of temperature changes between China and North-hemisphere.

English Abstract

YANG Bao, SHI Ya-feng, LI Heng-peng. CLIMATIC VARIATIONS IN CHINA OVER THE LAST 2000 YEARS[J]. 中国地理科学, 2001, 11(2): 97-103.
引用本文: YANG Bao, SHI Ya-feng, LI Heng-peng. CLIMATIC VARIATIONS IN CHINA OVER THE LAST 2000 YEARS[J]. 中国地理科学, 2001, 11(2): 97-103.
shu
YANG Bao, SHI Ya-feng, LI Heng-peng. CLIMATIC VARIATIONS IN CHINA OVER THE LAST 2000 YEARS[J]. Chinese Geographical Science, 2001, 11(2): 97-103.
Citation: YANG Bao, SHI Ya-feng, LI Heng-peng. CLIMATIC VARIATIONS IN CHINA OVER THE LAST 2000 YEARS[J]. Chinese Geographical Science, 2001, 11(2): 97-103.
shu

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