Synchronous timing of abrupt climate changes during the last glacial period

Author:

Corrick Ellen C.12ORCID,Drysdale Russell N.12ORCID,Hellstrom John C.3ORCID,Capron Emilie45ORCID,Rasmussen Sune Olander5ORCID,Zhang Xu678ORCID,Fleitmann Dominik9ORCID,Couchoud Isabelle21ORCID,Wolff Eric10ORCID

Affiliation:

1. School of Geography, The University of Melbourne, Melbourne, Victoria, Australia.

2. EDYTEM, CNRS, Université Savoie Mont Blanc, Université Grenoble Alpes, Chambéry, France.

3. School of Earth Science, The University of Melbourne, Melbourne, Victoria, Australia.

4. British Antarctic Survey, Cambridge, UK.

5. Physics of Ice, Climate and Earth, Niels Bohr Institute, University of Copenhagen, Copenhagen, Denmark.

6. Key Laboratory of Western China’s Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Center for Pan Third Pole Environment (Pan-TPE), Lanzhou University, Lanzhou, 730000, China.

7. Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, D-27570 Bremerhaven, Germany.

8. CAS Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences (CAS), Beijing 100101, China.

9. Department of Environmental Sciences, University of Basel, 4056 Basel, Switzerland.

10. Department of Earth Sciences, University of Cambridge, Cambridge, UK.

Abstract

Abrupt climate changes during the last glacial period have been detected in a global array of palaeoclimate records, but our understanding of their absolute timing and regional synchrony is incomplete. Our compilation of 63 published, independently dated speleothem records shows that abrupt warmings in Greenland were associated with synchronous climate changes across the Asian Monsoon, South American Monsoon, and European-Mediterranean regions that occurred within decades. Together with the demonstration of bipolar synchrony in atmospheric response, this provides independent evidence of synchronous high-latitude–to-tropical coupling of climate changes during these abrupt warmings. Our results provide a globally coherent framework with which to validate model simulations of abrupt climate change and to constrain ice-core chronologies.

Funder

Royal Society

Australian Research Council

Swiss National Science Foundation

Qingdao National Laboratory for Marine Science and Technology

Carlsberg Foundation

Australian Government Research Training Program Scholarship

Marie Skłodowska-Curie grant

Helmholtz Postdoc Program

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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