Articles | Volume 17, issue 2
https://doi.org/10.5194/cp-17-565-2021
© Author(s) 2021. 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-17-565-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
04 Mar 2021
Research article | Highlight paper |
| 04 Mar 2021
| 04 Mar 2021
Cryptotephra from the Icelandic Veiðivötn 1477 CE eruption in a Greenland ice core: confirming the dating of volcanic events in the 1450s CE and assessing the eruption's climatic impact
Peter M. Abbott
CORRESPONDING AUTHOR
Climate and Environmental Physics and Oeschger Centre for Climate
Change Research, University of Bern, 3012 Bern, Switzerland
Gill Plunkett
Archaeology and Palaeoecology, School of Natural and Built
Environment, Queen's University Belfast, Belfast BT7 1NN, UK
Christophe Corona
Geolab, Université Clermont Auvergne, CNRS, 63000,
Clermont-Ferrand, France
Nathan J. Chellman
Desert Research Institute, Nevada System of Higher Education, Reno,
Nevada 89512, USA
Joseph R. McConnell
Desert Research Institute, Nevada System of Higher Education, Reno,
Nevada 89512, USA
John R. Pilcher
Archaeology and Palaeoecology, School of Natural and Built
Environment, Queen's University Belfast, Belfast BT7 1NN, UK
Markus Stoffel
Climatic Change Impacts and Risks in the Anthropocene (C-CIA),
Institute for Environmental Sciences, University of Geneva, 1205 Geneva, Switzerland
Department of Earth Sciences, University of Geneva, 1205 Geneva,
Switzerland
Department F.-A. Forel for Environmental and Aquatic Sciences,
University of Geneva, 1205 Geneva, Switzerland
Michael Sigl
Climate and Environmental Physics and Oeschger Centre for Climate
Change Research, University of Bern, 3012 Bern, Switzerland
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Cited
16 citations as recorded by crossref.
- The 852/3 CE Mount Churchill eruption: examining the potential climatic and societal impacts and the timing of the Medieval Climate Anomaly in the North Atlantic region H. Mackay et al. 10.5194/cp-18-1475-2022
- Forced changes in the Pacific Walker circulation over the past millennium G. Falster et al. 10.1038/s41586-023-06447-0
- The significance of volcanic ash in Greenland ice cores during the Common Era G. Plunkett et al. 10.1016/j.quascirev.2022.107936
- Radiocarbon dating, magnitude, and catastrophic impact of Popocatépetl's Terminal Preclassic “Lorenzo pumice” Plinian eruption and paleomagnetic age constraints on the Nealtican lava flow field (central Mexico) C. Siebe et al. 10.1016/j.jvolgeores.2023.107974
- Environmental Changes in Antarctica Using a Shallow Ice Core from Dronning Maud Land (DML), East Antarctica A. Verma et al. 10.1007/s40710-023-00635-w
- Volcanic climate forcing preceding the inception of the Younger Dryas: Implications for tracing the Laacher See eruption P. Abbott et al. 10.1016/j.quascirev.2021.107260
- Climatic, weather, and socio-economic conditions corresponding to the mid-17th-century eruption cluster M. Stoffel et al. 10.5194/cp-18-1083-2022
- 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
- Mid-to Late Holocene East Antarctic ice-core tephrochronology: Implications for reconstructing volcanic eruptions and assessing their climatic impacts over the last 5,500 years P. Abbott et al. 10.1016/j.quascirev.2024.108544
- The unidentified eruption of 1809: a climatic cold case C. Timmreck et al. 10.5194/cp-17-1455-2021
- Fennoscandian tree-ring anatomy shows a warmer modern than medieval climate J. Björklund et al. 10.1038/s41586-023-06176-4
- High sensitivity of summer temperatures to stratospheric sulfur loading from volcanoes in the Northern Hemisphere A. Burke et al. 10.1073/pnas.2221810120
- No evidence for tephra in Greenland from the historic eruption of Vesuvius in 79 CE: implications for geochronology and paleoclimatology G. Plunkett et al. 10.5194/cp-18-45-2022
- 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
- Decadal-to-centennial increases of volcanic aerosols from Iceland challenge the concept of a Medieval Quiet Period I. Gabriel et al. 10.1038/s43247-024-01350-6
- Volcanic stratospheric sulfur injections and aerosol optical depth during the Holocene (past 11 500 years) from a bipolar ice-core array M. Sigl et al. 10.5194/essd-14-3167-2022
16 citations as recorded by crossref.
- The 852/3 CE Mount Churchill eruption: examining the potential climatic and societal impacts and the timing of the Medieval Climate Anomaly in the North Atlantic region H. Mackay et al. 10.5194/cp-18-1475-2022
- Forced changes in the Pacific Walker circulation over the past millennium G. Falster et al. 10.1038/s41586-023-06447-0
- The significance of volcanic ash in Greenland ice cores during the Common Era G. Plunkett et al. 10.1016/j.quascirev.2022.107936
- Radiocarbon dating, magnitude, and catastrophic impact of Popocatépetl's Terminal Preclassic “Lorenzo pumice” Plinian eruption and paleomagnetic age constraints on the Nealtican lava flow field (central Mexico) C. Siebe et al. 10.1016/j.jvolgeores.2023.107974
- Environmental Changes in Antarctica Using a Shallow Ice Core from Dronning Maud Land (DML), East Antarctica A. Verma et al. 10.1007/s40710-023-00635-w
- Volcanic climate forcing preceding the inception of the Younger Dryas: Implications for tracing the Laacher See eruption P. Abbott et al. 10.1016/j.quascirev.2021.107260
- Climatic, weather, and socio-economic conditions corresponding to the mid-17th-century eruption cluster M. Stoffel et al. 10.5194/cp-18-1083-2022
- 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
- Mid-to Late Holocene East Antarctic ice-core tephrochronology: Implications for reconstructing volcanic eruptions and assessing their climatic impacts over the last 5,500 years P. Abbott et al. 10.1016/j.quascirev.2024.108544
- The unidentified eruption of 1809: a climatic cold case C. Timmreck et al. 10.5194/cp-17-1455-2021
- Fennoscandian tree-ring anatomy shows a warmer modern than medieval climate J. Björklund et al. 10.1038/s41586-023-06176-4
- High sensitivity of summer temperatures to stratospheric sulfur loading from volcanoes in the Northern Hemisphere A. Burke et al. 10.1073/pnas.2221810120
- No evidence for tephra in Greenland from the historic eruption of Vesuvius in 79 CE: implications for geochronology and paleoclimatology G. Plunkett et al. 10.5194/cp-18-45-2022
- 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
- Decadal-to-centennial increases of volcanic aerosols from Iceland challenge the concept of a Medieval Quiet Period I. Gabriel et al. 10.1038/s43247-024-01350-6
- Volcanic stratospheric sulfur injections and aerosol optical depth during the Holocene (past 11 500 years) from a bipolar ice-core array M. Sigl et al. 10.5194/essd-14-3167-2022
Discussed (final revised paper)
Latest update: 16 Nov 2024
Short summary
Volcanic eruptions are a key source of climatic variability, and greater understanding of their past influence will increase the accuracy of future projections. We use volcanic ash from a 1477 CE Icelandic eruption in a Greenlandic ice core as a temporal fix point to constrain the timing of two eruptions in the 1450s CE and their climatic impact. Despite being the most explosive Icelandic eruption in the last 1200 years, the 1477 CE event had a limited impact on Northern Hemisphere climate.
Volcanic eruptions are a key source of climatic variability, and greater understanding of their...
