Articles | Volume 15, issue 2
https://doi.org/10.5194/cp-15-811-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-15-811-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
25 Apr 2019
Research article |
| 25 Apr 2019
| 25 Apr 2019
Decadal-scale progression of the onset of Dansgaard–Oeschger warming events
Climate and Environmental Physics, Physics Institute & Oeschger Center for Climate Change Research, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland
Emilie Capron
Physics of Ice, Climate and Earth, Niels Bohr Institute, University of Copenhagen, Tagensvej
16, 2200 Copenhagen, Denmark
British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UK
Sune Olander Rasmussen
Physics of Ice, Climate and Earth, Niels Bohr Institute, University of Copenhagen, Tagensvej
16, 2200 Copenhagen, Denmark
Simon Schüpbach
Climate and Environmental Physics, Physics Institute & Oeschger Center for Climate Change Research, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland
Matthias Bigler
Climate and Environmental Physics, Physics Institute & Oeschger Center for Climate Change Research, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland
Florian Adolphi
Climate and Environmental Physics, Physics Institute & Oeschger Center for Climate Change Research, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland
Quaternary Sciences, Department of Geology, Lund University, Sölvegatan 12, 22362 Lund, Sweden
Hubertus Fischer
Climate and Environmental Physics, Physics Institute & Oeschger Center for Climate Change Research, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland
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- Dansgaard-Oeschger and Heinrich event temperature anomalies in the North Atlantic set by sea ice, frontal position and thermocline structure J. Pedro et al. 10.1016/j.quascirev.2022.107599
- Ice and ocean constraints on early human migrations into North America along the Pacific coast S. Praetorius et al. 10.1073/pnas.2208738120
- Continuous synchronization of the Greenland ice-core and U–Th timescales using probabilistic inversion F. Muschitiello & M. Aquino-Lopez 10.5194/cp-20-1415-2024
- Bipolar impact and phasing of Heinrich-type climate variability K. Martin et al. 10.1038/s41586-023-05875-2
- Prediction of Dansgaard‐Oeschger Events From Greenland Dust Records J. Lohmann 10.1029/2019GL085133
- Formal subdivision of the Quaternary System/Period: Present status and future directions M. Head 10.1016/j.quaint.2019.05.018
- The anatomy of past abrupt warmings recorded in Greenland ice E. Capron et al. 10.1038/s41467-021-22241-w
- Ice core evidence for major volcanic eruptions at the onset of Dansgaard–Oeschger warming events J. Lohmann & A. Svensson 10.5194/cp-18-2021-2022
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- Coupled atmosphere-ice-ocean dynamics during Heinrich Stadial 2 X. Dong et al. 10.1038/s41467-022-33583-4
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- Abrupt climate change as a rate-dependent cascading tipping point J. Lohmann et al. 10.5194/esd-12-819-2021
- The PaleoJump database for abrupt transitions in past climates W. Bagniewski et al. 10.1038/s41598-023-30592-1
- Ecosystem Resilience Monitoring and Early Warning Using Earth Observation Data: Challenges and Outlook S. Bathiany et al. 10.1007/s10712-024-09833-z
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- Greenland Ice Core Record of Last Glacial Dust Sources and Atmospheric Circulation G. Újvári et al. 10.1029/2022JD036597
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- NALPS19: sub-orbital-scale climate variability recorded in northern Alpine speleothems during the last glacial period G. Moseley et al. 10.5194/cp-16-29-2020
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Latest update: 26 Jul 2024
Short summary
The cause of the rapid warming events documented in proxy records across the Northern Hemisphere during the last glacial has been a long-standing puzzle in paleo-climate research. Here, we use high-resolution ice-core data from to cores in Greenland to investigate the progression during the onset of these events on multi-annual timescales to test their plausible triggers. We show that atmospheric circulation changes preceded the warming in Greenland and the collapse of the sea ice by a decade.
The cause of the rapid warming events documented in proxy records across the Northern Hemisphere...
