Climatic, weather, and socio-economic conditions corresponding to the mid-17th-century eruption cluster ...
The mid-17th century is characterized by a cluster of explosive volcanic eruptions in the 1630s and 1640s, climatic conditions culminating in the Maunder Minimum as well as political instability and famine in regions of Western and Northern Europe as well as China and Japan. This contribution invest...
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ftdatacite:10.48350/170175 2024-09-15T17:48:55+00:00 Climatic, weather, and socio-economic conditions corresponding to the mid-17th-century eruption cluster ... Stoffel, Markus Corona, Christophe Ludlow, Francis Sigl, Michael Huhtamaa, Heli Garnier, Emmanuel Helama, Samuli Guillet, Sébastien Crampsie, Arlene Kleemann, Katrin Camenisch, Chantal McConnell, Joseph Gao, Chaochao 2022 https://dx.doi.org/10.48350/170175 https://boris.unibe.ch/170175/ unknown Copernicus Publications https://dx.doi.org/10.5194/cp-18-1083-2022 open access Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 570 Life sciences; biology 300 Social sciences, sociology & anthropology 530 Physics 540 Chemistry 550 Earth sciences & geology 940 History of Europe 950 History of Asia Text ScholarlyArticle article-journal journal article 2022 ftdatacite https://doi.org/10.48350/17017510.5194/cp-18-1083-2022 2024-09-02T10:17:31Z The mid-17th century is characterized by a cluster of explosive volcanic eruptions in the 1630s and 1640s, climatic conditions culminating in the Maunder Minimum as well as political instability and famine in regions of Western and Northern Europe as well as China and Japan. This contribution investigates the sources of the eruptions of the 1630s and 1640s and their possible impact on contemporary climate using ice-core, tree-ring and historical evidence, but will also look into the socio-political context in which they occurred and the human responses they may have triggered. Three distinct sulfur peaks are found in the Greenland ice core record in 1637, 1641-42 and 1646. In Antarctica, only one unambiguous sulfate spike is recorded, peaking in 1642. The resulting bipolar sulfur peak in 1641-1642 can likely be ascribed to the eruption of Mount Parker (6°N, Philippines) on December 26, 1640, but sulfate emitted from Koma-ga-take (42°N, Japan) volcano on July 31, 1641, has potentially also contributed to the ... Text Antarc* Antarctica Greenland Greenland ice core ice core DataCite |
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unknown |
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570 Life sciences; biology 300 Social sciences, sociology & anthropology 530 Physics 540 Chemistry 550 Earth sciences & geology 940 History of Europe 950 History of Asia |
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570 Life sciences; biology 300 Social sciences, sociology & anthropology 530 Physics 540 Chemistry 550 Earth sciences & geology 940 History of Europe 950 History of Asia Stoffel, Markus Corona, Christophe Ludlow, Francis Sigl, Michael Huhtamaa, Heli Garnier, Emmanuel Helama, Samuli Guillet, Sébastien Crampsie, Arlene Kleemann, Katrin Camenisch, Chantal McConnell, Joseph Gao, Chaochao Climatic, weather, and socio-economic conditions corresponding to the mid-17th-century eruption cluster ... |
topic_facet |
570 Life sciences; biology 300 Social sciences, sociology & anthropology 530 Physics 540 Chemistry 550 Earth sciences & geology 940 History of Europe 950 History of Asia |
description |
The mid-17th century is characterized by a cluster of explosive volcanic eruptions in the 1630s and 1640s, climatic conditions culminating in the Maunder Minimum as well as political instability and famine in regions of Western and Northern Europe as well as China and Japan. This contribution investigates the sources of the eruptions of the 1630s and 1640s and their possible impact on contemporary climate using ice-core, tree-ring and historical evidence, but will also look into the socio-political context in which they occurred and the human responses they may have triggered. Three distinct sulfur peaks are found in the Greenland ice core record in 1637, 1641-42 and 1646. In Antarctica, only one unambiguous sulfate spike is recorded, peaking in 1642. The resulting bipolar sulfur peak in 1641-1642 can likely be ascribed to the eruption of Mount Parker (6°N, Philippines) on December 26, 1640, but sulfate emitted from Koma-ga-take (42°N, Japan) volcano on July 31, 1641, has potentially also contributed to the ... |
format |
Text |
author |
Stoffel, Markus Corona, Christophe Ludlow, Francis Sigl, Michael Huhtamaa, Heli Garnier, Emmanuel Helama, Samuli Guillet, Sébastien Crampsie, Arlene Kleemann, Katrin Camenisch, Chantal McConnell, Joseph Gao, Chaochao |
author_facet |
Stoffel, Markus Corona, Christophe Ludlow, Francis Sigl, Michael Huhtamaa, Heli Garnier, Emmanuel Helama, Samuli Guillet, Sébastien Crampsie, Arlene Kleemann, Katrin Camenisch, Chantal McConnell, Joseph Gao, Chaochao |
author_sort |
Stoffel, Markus |
title |
Climatic, weather, and socio-economic conditions corresponding to the mid-17th-century eruption cluster ... |
title_short |
Climatic, weather, and socio-economic conditions corresponding to the mid-17th-century eruption cluster ... |
title_full |
Climatic, weather, and socio-economic conditions corresponding to the mid-17th-century eruption cluster ... |
title_fullStr |
Climatic, weather, and socio-economic conditions corresponding to the mid-17th-century eruption cluster ... |
title_full_unstemmed |
Climatic, weather, and socio-economic conditions corresponding to the mid-17th-century eruption cluster ... |
title_sort |
climatic, weather, and socio-economic conditions corresponding to the mid-17th-century eruption cluster ... |
publisher |
Copernicus Publications |
publishDate |
2022 |
url |
https://dx.doi.org/10.48350/170175 https://boris.unibe.ch/170175/ |
genre |
Antarc* Antarctica Greenland Greenland ice core ice core |
genre_facet |
Antarc* Antarctica Greenland Greenland ice core ice core |
op_relation |
https://dx.doi.org/10.5194/cp-18-1083-2022 |
op_rights |
open access Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 |
op_doi |
https://doi.org/10.48350/17017510.5194/cp-18-1083-2022 |
_version_ |
1810290552744181760 |