Lunar eclipses illuminate timing and climate impact of medieval volcanism
Acknowledgements: S.G., C.C., M.K. and M. Stoffel were supported by the Swiss National Science Foundation Sinergia Project CALDERA (CRSII5_183571). S.G. acknowledges A. Harrak (Department of Near and Middle Eastern Civilizations, University of Toronto), F. Espenak (NASA Goddard Space Flight Center),...
Main Authors: | , , , , , , , , , , , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Nature Publishing Group UK
2023
|
Subjects: | |
Online Access: | https://doi.org/10.17863/CAM.96139 https://www.repository.cam.ac.uk/handle/1810/348713 |
id |
ftunivcam:oai:www.repository.cam.ac.uk:1810/348713 |
---|---|
record_format |
openpolar |
spelling |
ftunivcam:oai:www.repository.cam.ac.uk:1810/348713 2023-07-30T04:04:10+02:00 Lunar eclipses illuminate timing and climate impact of medieval volcanism Guillet, Sébastien Corona, Christophe Oppenheimer, Clive Lavigne, Franck Khodri, Myriam Ludlow, Francis Sigl, Michael Toohey, Matthew Atkins, Paul S. Yang, Zhen Muranaka, Tomoko Horikawa, Nobuko Stoffel, Markus 2023-04-17T15:00:35Z application/pdf text/xml application/zip https://doi.org/10.17863/CAM.96139 https://www.repository.cam.ac.uk/handle/1810/348713 en eng Nature Publishing Group UK Nature doi:10.17863/CAM.96139 https://www.repository.cam.ac.uk/handle/1810/348713 Article /704/106/694/1108 /704/106/413 Article 2023 ftunivcam https://doi.org/10.17863/CAM.96139 2023-07-10T21:57:17Z Acknowledgements: S.G., C.C., M.K. and M. Stoffel were supported by the Swiss National Science Foundation Sinergia Project CALDERA (CRSII5_183571). S.G. acknowledges A. Harrak (Department of Near and Middle Eastern Civilizations, University of Toronto), F. Espenak (NASA Goddard Space Flight Center), F. Hierink (Institute for Environmental Sciences, University of Geneva) and P. Souyri (Department of East Asian Studies, University of Geneva) for providing advice on the manuscript. F. Lavigne was supported by Institut Universitaire de France (IUF, Academic Institute of France). M.K. received funding from the EUR IPSL – Climate Graduate School project, managed by the ANR within the “Investissements d’avenir” programme under reference ANR-11-IDEX-0004-17-EURE-0006. F. Ludlow received funding from an Irish Research Council Starting Laureate Award (CLICAB project, IRCLA/2017/303). F. Ludlow and Z.Y. also received funding from a European Research Council (ERC) Synergy Grant (4-OCEANS; grant agreement no. 951649) under the European Union’s Horizon 2020 research and innovation programme. M. Sigl received funding from the ERC under the European Union’s Horizon 2020 research and innovation programme (grant agreement no. 820047). This paper is a product of the Volcanic Impacts on Climate and Society (VICS) working group. Explosive volcanism is a key contributor to climate variability on interannual to centennial timescales1. Understanding the far-field societal impacts of eruption-forced climatic changes requires firm event chronologies and reliable estimates of both the burden and altitude (that is, tropospheric versus stratospheric) of volcanic sulfate aerosol2, 3. However, despite progress in ice-core dating, uncertainties remain in these key factors4. This particularly hinders investigation of the role of large, temporally clustered eruptions during the High Medieval Period (HMP, 1100–1300 ce), which have been implicated in the transition from the warm Medieval Climate Anomaly to the Little Ice Age5. Here we shed new ... Article in Journal/Newspaper ice core Apollo - University of Cambridge Repository |
institution |
Open Polar |
collection |
Apollo - University of Cambridge Repository |
op_collection_id |
ftunivcam |
language |
English |
topic |
Article /704/106/694/1108 /704/106/413 |
spellingShingle |
Article /704/106/694/1108 /704/106/413 Guillet, Sébastien Corona, Christophe Oppenheimer, Clive Lavigne, Franck Khodri, Myriam Ludlow, Francis Sigl, Michael Toohey, Matthew Atkins, Paul S. Yang, Zhen Muranaka, Tomoko Horikawa, Nobuko Stoffel, Markus Lunar eclipses illuminate timing and climate impact of medieval volcanism |
topic_facet |
Article /704/106/694/1108 /704/106/413 |
description |
Acknowledgements: S.G., C.C., M.K. and M. Stoffel were supported by the Swiss National Science Foundation Sinergia Project CALDERA (CRSII5_183571). S.G. acknowledges A. Harrak (Department of Near and Middle Eastern Civilizations, University of Toronto), F. Espenak (NASA Goddard Space Flight Center), F. Hierink (Institute for Environmental Sciences, University of Geneva) and P. Souyri (Department of East Asian Studies, University of Geneva) for providing advice on the manuscript. F. Lavigne was supported by Institut Universitaire de France (IUF, Academic Institute of France). M.K. received funding from the EUR IPSL – Climate Graduate School project, managed by the ANR within the “Investissements d’avenir” programme under reference ANR-11-IDEX-0004-17-EURE-0006. F. Ludlow received funding from an Irish Research Council Starting Laureate Award (CLICAB project, IRCLA/2017/303). F. Ludlow and Z.Y. also received funding from a European Research Council (ERC) Synergy Grant (4-OCEANS; grant agreement no. 951649) under the European Union’s Horizon 2020 research and innovation programme. M. Sigl received funding from the ERC under the European Union’s Horizon 2020 research and innovation programme (grant agreement no. 820047). This paper is a product of the Volcanic Impacts on Climate and Society (VICS) working group. Explosive volcanism is a key contributor to climate variability on interannual to centennial timescales1. Understanding the far-field societal impacts of eruption-forced climatic changes requires firm event chronologies and reliable estimates of both the burden and altitude (that is, tropospheric versus stratospheric) of volcanic sulfate aerosol2, 3. However, despite progress in ice-core dating, uncertainties remain in these key factors4. This particularly hinders investigation of the role of large, temporally clustered eruptions during the High Medieval Period (HMP, 1100–1300 ce), which have been implicated in the transition from the warm Medieval Climate Anomaly to the Little Ice Age5. Here we shed new ... |
format |
Article in Journal/Newspaper |
author |
Guillet, Sébastien Corona, Christophe Oppenheimer, Clive Lavigne, Franck Khodri, Myriam Ludlow, Francis Sigl, Michael Toohey, Matthew Atkins, Paul S. Yang, Zhen Muranaka, Tomoko Horikawa, Nobuko Stoffel, Markus |
author_facet |
Guillet, Sébastien Corona, Christophe Oppenheimer, Clive Lavigne, Franck Khodri, Myriam Ludlow, Francis Sigl, Michael Toohey, Matthew Atkins, Paul S. Yang, Zhen Muranaka, Tomoko Horikawa, Nobuko Stoffel, Markus |
author_sort |
Guillet, Sébastien |
title |
Lunar eclipses illuminate timing and climate impact of medieval volcanism |
title_short |
Lunar eclipses illuminate timing and climate impact of medieval volcanism |
title_full |
Lunar eclipses illuminate timing and climate impact of medieval volcanism |
title_fullStr |
Lunar eclipses illuminate timing and climate impact of medieval volcanism |
title_full_unstemmed |
Lunar eclipses illuminate timing and climate impact of medieval volcanism |
title_sort |
lunar eclipses illuminate timing and climate impact of medieval volcanism |
publisher |
Nature Publishing Group UK |
publishDate |
2023 |
url |
https://doi.org/10.17863/CAM.96139 https://www.repository.cam.ac.uk/handle/1810/348713 |
genre |
ice core |
genre_facet |
ice core |
op_relation |
doi:10.17863/CAM.96139 https://www.repository.cam.ac.uk/handle/1810/348713 |
op_doi |
https://doi.org/10.17863/CAM.96139 |
_version_ |
1772815379904593920 |