Articles | Volume 15, issue 3
https://doi.org/10.5194/cp-15-913-2019
© 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-15-913-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Antarctic temperature and CO2: near-synchrony yet variable phasing during the last deglaciation
Jai Chowdhry Beeman
Université Grenoble Alpes, CNRS, IRD, IGE, 38000 Grenoble, France
Léa Gest
Université Grenoble Alpes, CNRS, IRD, IGE, 38000 Grenoble, France
Frédéric Parrenin
CORRESPONDING AUTHOR
Université Grenoble Alpes, CNRS, IRD, IGE, 38000 Grenoble, France
Dominique Raynaud
Université Grenoble Alpes, CNRS, IRD, IGE, 38000 Grenoble, France
Tyler J. Fudge
Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195, USA
Christo Buizert
College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA
Edward J. Brook
College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA
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- Stochastic assessment of temperature–CO<sub>2</sub> causal relationship in climate from the Phanerozoic through modern times D. Koutsoyiannis 10.3934/mbe.2024287
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- Southern Ocean glacial conditions and their influence on deglacial events E. Sikes et al. 10.1038/s43017-023-00436-7
- Late Quaternary climatic inferences from southern Patagonia (∼53°S): A holistic palaeoecological approach to tracking the behaviour of the southern westerly winds R. McCulloch et al. 10.1016/j.palaeo.2023.111822
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- Climate Variations in the Antarctic Region on a Long Time Scale and Current Climate Changes V. Dergachev 10.1134/S0016793223080066
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Discussed (final revised paper)
Discussed (preprint)
Latest update: 22 Nov 2024
Short summary
Atmospheric CO2 was likely an important amplifier of global-scale orbitally-driven warming during the last deglaciation. However, the mechanisms responsible for the rise in CO2, and the coherent rise in Antarctic isotopic temperature records, are under debate. Using a stochastic method, we detect variable lags between coherent changes in Antarctic temperature and CO2. This implies that the climate mechanisms linking the two records changed or experienced modulations during the deglaciation.
Atmospheric CO2 was likely an important amplifier of global-scale orbitally-driven warming...