Articles | Volume 18, issue 3
https://doi.org/10.5194/cp-18-485-2022
© Author(s) 2022. 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-18-485-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
15 Mar 2022
Research article | Highlight paper |
| 15 Mar 2022
| 15 Mar 2022
Magnitude, frequency and climate forcing of global volcanism during the last glacial period as seen in Greenland and Antarctic ice cores (60–9 ka)
Physics of Ice, Climate and Earth, Niels Bohr Institute, University of Copenhagen, 2100, Denmark
Physics of Ice, Climate and Earth, Niels Bohr Institute, University of Copenhagen, 2100, Denmark
Christine S. Hvidberg
Physics of Ice, Climate and Earth, Niels Bohr Institute, University of Copenhagen, 2100, Denmark
Johannes Lohmann
Physics of Ice, Climate and Earth, Niels Bohr Institute, University of Copenhagen, 2100, Denmark
Steffen Kristiansen
Physics of Ice, Climate and Earth, Niels Bohr Institute, University of Copenhagen, 2100, Denmark
Dorthe Dahl-Jensen
Physics of Ice, Climate and Earth, Niels Bohr Institute, University of Copenhagen, 2100, Denmark
Centre for Earth Observation Science, University of Manitoba, Winnipeg, Manitoba, R3T 2N2, Canada
Jørgen Peder Steffensen
Physics of Ice, Climate and Earth, Niels Bohr Institute, University of Copenhagen, 2100, Denmark
Sune Olander Rasmussen
Physics of Ice, Climate and Earth, Niels Bohr Institute, University of Copenhagen, 2100, Denmark
Eliza Cook
Physics of Ice, Climate and Earth, Niels Bohr Institute, University of Copenhagen, 2100, Denmark
Helle Astrid Kjær
Physics of Ice, Climate and Earth, Niels Bohr Institute, University of Copenhagen, 2100, Denmark
Bo M. Vinther
Physics of Ice, Climate and Earth, Niels Bohr Institute, University of Copenhagen, 2100, Denmark
Hubertus Fischer
Climate and Environmental Physics, Physics Institute and Oeschger Center for Climate Change Research, University of Bern, Sidlerstrasse 5, Bern, Switzerland
Thomas Stocker
Climate and Environmental Physics, Physics Institute and Oeschger Center for Climate Change Research, University of Bern, Sidlerstrasse 5, Bern, Switzerland
Michael Sigl
Climate and Environmental Physics, Physics Institute and Oeschger Center for Climate Change Research, University of Bern, Sidlerstrasse 5, Bern, Switzerland
Matthias Bigler
Climate and Environmental Physics, Physics Institute and Oeschger Center for Climate Change Research, University of Bern, Sidlerstrasse 5, Bern, Switzerland
Mirko Severi
Department of Chemistry, University of Florence, Florence, Italy
Rita Traversi
Department of Chemistry, University of Florence, Florence, Italy
Robert Mulvaney
British Antarctic Survey, Cambridge, UK
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- Food system adaptation and maintaining trade could mitigate global famine in abrupt sunlight reduction scenarios M. Rivers et al. 10.1016/j.gfs.2024.100807
- Effective diffusivity of sulfuric acid in Antarctic ice cores T. Fudge et al. 10.5194/cp-20-297-2024
- Disparate energy sources for slow and fast Dansgaard–Oeschger cycles D. Liebrand et al. 10.5194/cp-19-1447-2023
- A sulfur and halogen budget for the large magmatic system beneath Taupō volcano M. Sharpe et al. 10.1007/s00410-022-01959-w
- Ice-core data used for the construction of the Greenland Ice-Core Chronology 2005 and 2021 (GICC05 and GICC21) S. Rasmussen et al. 10.5194/essd-15-3351-2023
- Impact of the Tambora volcanic eruption of 1815 on islands and relevance to future sunlight-blocking catastrophes N. Wilson et al. 10.1038/s41598-023-30729-2
- State-dependent impact of major volcanic eruptions observed in ice-core records of the last glacial period J. Lohmann et al. 10.5194/cp-20-313-2024
- The Ethics of Volcano Geoengineering M. Cassidy et al. 10.1029/2023EF003714
- Volcanism and the Greenland ice cores: A new tephrochronological framework for the last glacial-interglacial transition (LGIT) based on cryptotephra deposits in three ice cores E. Cook et al. 10.1016/j.quascirev.2022.107596
- Canadian forest fires, Icelandic volcanoes and increased local dust observed in six shallow Greenland firn cores H. Kjær et al. 10.5194/cp-18-2211-2022
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- A multi-ice-core, annual-layer-counted Greenland ice-core chronology for the last 3800 years: GICC21 G. Sinnl et al. 10.5194/cp-18-1125-2022
- Volcanic glass from the 1.8 ka Taupō eruption (New Zealand) detected in Antarctic ice at ~ 230 CE S. Piva et al. 10.1038/s41598-023-42602-3
- An assessment of potential causal links between deglaciation and eruption rates at arc volcanoes C. Conway et al. 10.3389/feart.2023.1082342
- Bipolar ice-core records constrain possible dates and global radiative forcing following the ∼74 ka Toba eruption J. Lin et al. 10.1016/j.quascirev.2023.108162
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- A Cryptotephra Layer in Sediments of an Infilled Maar Lake from the Eifel (Germany): First Evidence of Campanian Ignimbrite Ash Airfall in Central Europe F. Schenk et al. 10.3390/quat7020017
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- Frequency of large volcanic eruptions over the past 200 000 years E. Wolff et al. 10.5194/cp-19-23-2023
- The next massive volcano eruption will cause climate chaos — and we are unprepared M. Stoffel et al. 10.1038/d41586-024-03680-z
- Huge volcanic eruptions: time to prepare M. Cassidy & L. Mani 10.1038/d41586-022-02177-x
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Discussed (final revised paper)
Latest update: 13 Dec 2024
Short summary
We employ acidity records from Greenland and Antarctic ice cores to estimate the emission strength, frequency and climatic forcing for large volcanic eruptions from the last half of the last glacial period. A total of 25 volcanic eruptions are found to be larger than any eruption in the last 2500 years, and we identify more eruptions than obtained from geological evidence. Towards the end of the glacial period, there is a notable increase in volcanic activity observed for Greenland.
We employ acidity records from Greenland and Antarctic ice cores to estimate the emission...
