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Coupled atmosphere-ice-ocean dynamics during Heinrich Stadial 2

Author

Listed:
  • Xiyu Dong

    (Xi’an Jiaotong University)

  • Gayatri Kathayat

    (Xi’an Jiaotong University)

  • Sune O. Rasmussen

    (University of Copenhagen)

  • Anders Svensson

    (University of Copenhagen)

  • Jeffrey P. Severinghaus

    (University of California San Diego)

  • Hanying Li

    (Xi’an Jiaotong University)

  • Ashish Sinha

    (Xi’an Jiaotong University
    California State University)

  • Yao Xu

    (Xi’an Jiaotong University)

  • Haiwei Zhang

    (Xi’an Jiaotong University)

  • Zhengguo Shi

    (Xi’an Jiaotong University
    Chinese Academy of Sciences
    Chinese Academy of Sciences)

  • Yanjun Cai

    (Xi’an Jiaotong University)

  • Carlos Pérez-Mejías

    (Xi’an Jiaotong University)

  • Jonathan Baker

    (Xi’an Jiaotong University)

  • Jingyao Zhao

    (Xi’an Jiaotong University)

  • Christoph Spötl

    (University of Innsbruck)

  • Andrea Columbu

    (University of Pisa)

  • Youfeng Ning

    (Xi’an Jiaotong University)

  • Nicolás M. Stríkis

    (Universidade Federal Fluminense)

  • Shitao Chen

    (Nanjing Normal University
    Key Laboratory of Virtual Geographic Environment (Nanjing Normal University), Ministry of Education
    Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application)

  • Xianfeng Wang

    (Nanyang Technological University)

  • Anil K. Gupta

    (Indian Institute of Technology Kharagpur)

  • Som Dutt

    (Wadia Institute of Himalayan Geology)

  • Fan Zhang

    (Xi’an Jiaotong University)

  • Francisco W. Cruz

    (Universidade de São Paulo)

  • Zhisheng An

    (Chinese Academy of Sciences)

  • R. Lawrence Edwards

    (University of Minnesota)

  • Hai Cheng

    (Xi’an Jiaotong University
    Chinese Academy of Sciences
    MLR, Institute of Karst Geology, CAGS)

Abstract

Our understanding of climate dynamics during millennial-scale events is incomplete, partially due to the lack of their precise phase analyses under various boundary conditions. Here we present nine speleothem oxygen-isotope records from mid-to-low-latitude monsoon regimes with sub-centennial age precision and multi-annual resolution, spanning the Heinrich Stadial 2 (HS2) — a millennial-scale event that occurred at the Last Glacial Maximum. Our data suggests that the Greenland and Antarctic ice-core chronologies require +320- and +400-year adjustments, respectively, supported by extant volcanic evidence and radiocarbon ages. Our chronological framework shows a synchronous HS2 onset globally. Our records precisely characterize a centennial-scale abrupt “tropical atmospheric seesaw” superimposed on the conventional “bipolar seesaw” at the beginning of HS2, implying a unique response/feedback from low-latitude hydroclimate. Together with our observation of an early South American monsoon shift at the HS2 termination, we suggest a more active role of low-latitude hydroclimate dynamics underlying millennial events than previously thought.

Suggested Citation

  • Xiyu Dong & Gayatri Kathayat & Sune O. Rasmussen & Anders Svensson & Jeffrey P. Severinghaus & Hanying Li & Ashish Sinha & Yao Xu & Haiwei Zhang & Zhengguo Shi & Yanjun Cai & Carlos Pérez-Mejías & Jon, 2022. "Coupled atmosphere-ice-ocean dynamics during Heinrich Stadial 2," Nature Communications, Nature, vol. 13(1), pages 1-14, December.
  • Handle: RePEc:nat:natcom:v:13:y:2022:i:1:d:10.1038_s41467-022-33583-4
    DOI: 10.1038/s41467-022-33583-4
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    References listed on IDEAS

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