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Climate Dynamics

, Volume 48, Issue 5–6, pp 1769–1778 | Cite as

Decreasing monsoon precipitation in southwest China during the last 240 years associated with the warming of tropical ocean

  • Liangcheng Tan
  • Yanjun Cai
  • Zhisheng An
  • Hai Cheng
  • Chuan-Chou Shen
  • Yongli Gao
  • R. Lawrence Edwards
Article

Abstract

Based on an absolutely dated stalagmite δ18O record from Yunnan province, China, we reconstructed monsoon precipitation variations in southwest China since 1760 AD with a resolution of about 2 years. Combining the speleothem δ18O and observed rainfall records, we find an overall decreasing trend in monsoon precipitation in this region and suggest that the recent drought in 2009–2012 AD has been the driest since 1760 AD. Our speleothem record is consistent with the monsoon precipitation records reconstructed from tree rings in the Nepal Himalaya and southeastern Tibetan Plateau. However, it is anti-correlated with a speleothem record from central India, which confirms the observed anti-phase variations of Indian monsoon precipitation with moistures from the Bay of Bengal and Arabian Sea on multi-decadal to centennial timescales during historical time. The long-term warming of tropical ocean may have caused the decrease of the land-sea thermal gradient and the amount of moisture transported from the Bay of Bengal, which may reduce precipitations in southwest China during the last 240 years. On decadal scale, El Nińo-like conditions of tropical Pacific sea surface temperature may cause drought in this region. Climate model simulations suggest El Niño-like conditions exist in tropical Pacific under global warming scenarios. As a result, it is crucial to have adaptive strategies to overcome future declines in precipitation and/or drought events in southwest China.

Keywords

Drought Southwest China Tropical SST El Niño Stalagmite 

Notes

Acknowledgments

The final version of the manuscript benefited for constructive suggestions from three anonymous reviewers. We gratefully acknowledge the National Key Basic Research Program of China (2013CB955902), National Natural Science Foundation of China (41372192; 41230524), West Light Foundation of Chinese Academy of Sciences, and Youth Innovation Promotion Association of Chinese Academy of Sciences (2012295) for funding this research. C.-C. Shen received financial support from MOST (104-2119-M-002-003). H. Cheng and R. L. Edwards received financial support from the U.S. NSF (EAR-0908792 and EAR-1211299).

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Copyright information

© Springer-Verlag Berlin Heidelberg 2016

Authors and Affiliations

  • Liangcheng Tan
    • 1
    • 2
    • 3
  • Yanjun Cai
    • 1
    • 2
  • Zhisheng An
    • 1
    • 2
  • Hai Cheng
    • 2
    • 4
  • Chuan-Chou Shen
    • 5
  • Yongli Gao
    • 6
  • R. Lawrence Edwards
    • 4
  1. 1.State Key Laboratory of Loess and Quaternary Geology, Institute of Earth EnvironmentChinese Academy of SciencesXi’anChina
  2. 2.Institute of Global Environmental ChangeXi’an Jiaotong UniversityXi’anChina
  3. 3.Joint Center for Global Change Studies (JCGCS)BeijingChina
  4. 4.Department of Earth SciencesUniversity of MinnesotaMinneapolisUSA
  5. 5.High-Precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of GeosciencesNational Taiwan UniversityTaipeiTaiwan
  6. 6.Department of Geological Sciences, Center for Water ResearchUniversity of Texas at San AntonioSan AntonioUSA

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