Tree-ring and summer-temperature response to volcanic aerosol forcing at the northern tree-line, Kola Peninsula, Russia
Potential linkages between volcanic activity and a 403-year record of Pinus sylvestris L. (Scots pine) growth and summer temperatures estimated from tree-ring widths are evaluated from an Arctic tree-line site on the Kola Peninsula, northwestern Russia. The joint occurrence of volcanic eruptions and...
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Language: | English |
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Online Access: | http://dx.doi.org/10.1191/095968301678302940 http://journals.sagepub.com/doi/pdf/10.1191/095968301678302940 |
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crsagepubl:10.1191/095968301678302940 2023-05-15T15:03:31+02:00 Tree-ring and summer-temperature response to volcanic aerosol forcing at the northern tree-line, Kola Peninsula, Russia Gervais, Bruce R. MacDonald, Glen M. 2001 http://dx.doi.org/10.1191/095968301678302940 http://journals.sagepub.com/doi/pdf/10.1191/095968301678302940 en eng SAGE Publications http://journals.sagepub.com/page/policies/text-and-data-mining-license The Holocene volume 11, issue 4, page 499-505 ISSN 0959-6836 1477-0911 Paleontology Earth-Surface Processes Ecology Archeology Global and Planetary Change journal-article 2001 crsagepubl https://doi.org/10.1191/095968301678302940 2022-05-26T08:12:52Z Potential linkages between volcanic activity and a 403-year record of Pinus sylvestris L. (Scots pine) growth and summer temperatures estimated from tree-ring widths are evaluated from an Arctic tree-line site on the Kola Peninsula, northwestern Russia. The joint occurrence of volcanic eruptions and severe negative ring-width values is more than four times that expected by chance. A composite average of temperatures indicates that a 0.72°C temperature reduction is typical for the year immediately following volcanic eruptions, while tree growth is reduced for up to two decades. The Greenland Ice Sheet Project 2 (GISP2) volcanic sulphate record shows a small but significant correlation with summer temperatures. Volcanic aerosols originating at low and middle latitudes appear to cause the greatest ring-width reduction and cooling. Article in Journal/Newspaper Arctic Greenland Greenland Ice Sheet Project Ice Sheet kola peninsula SAGE Publications (via Crossref) Arctic Greenland Kola Peninsula The Holocene 11 4 499 505 |
institution |
Open Polar |
collection |
SAGE Publications (via Crossref) |
op_collection_id |
crsagepubl |
language |
English |
topic |
Paleontology Earth-Surface Processes Ecology Archeology Global and Planetary Change |
spellingShingle |
Paleontology Earth-Surface Processes Ecology Archeology Global and Planetary Change Gervais, Bruce R. MacDonald, Glen M. Tree-ring and summer-temperature response to volcanic aerosol forcing at the northern tree-line, Kola Peninsula, Russia |
topic_facet |
Paleontology Earth-Surface Processes Ecology Archeology Global and Planetary Change |
description |
Potential linkages between volcanic activity and a 403-year record of Pinus sylvestris L. (Scots pine) growth and summer temperatures estimated from tree-ring widths are evaluated from an Arctic tree-line site on the Kola Peninsula, northwestern Russia. The joint occurrence of volcanic eruptions and severe negative ring-width values is more than four times that expected by chance. A composite average of temperatures indicates that a 0.72°C temperature reduction is typical for the year immediately following volcanic eruptions, while tree growth is reduced for up to two decades. The Greenland Ice Sheet Project 2 (GISP2) volcanic sulphate record shows a small but significant correlation with summer temperatures. Volcanic aerosols originating at low and middle latitudes appear to cause the greatest ring-width reduction and cooling. |
format |
Article in Journal/Newspaper |
author |
Gervais, Bruce R. MacDonald, Glen M. |
author_facet |
Gervais, Bruce R. MacDonald, Glen M. |
author_sort |
Gervais, Bruce R. |
title |
Tree-ring and summer-temperature response to volcanic aerosol forcing at the northern tree-line, Kola Peninsula, Russia |
title_short |
Tree-ring and summer-temperature response to volcanic aerosol forcing at the northern tree-line, Kola Peninsula, Russia |
title_full |
Tree-ring and summer-temperature response to volcanic aerosol forcing at the northern tree-line, Kola Peninsula, Russia |
title_fullStr |
Tree-ring and summer-temperature response to volcanic aerosol forcing at the northern tree-line, Kola Peninsula, Russia |
title_full_unstemmed |
Tree-ring and summer-temperature response to volcanic aerosol forcing at the northern tree-line, Kola Peninsula, Russia |
title_sort |
tree-ring and summer-temperature response to volcanic aerosol forcing at the northern tree-line, kola peninsula, russia |
publisher |
SAGE Publications |
publishDate |
2001 |
url |
http://dx.doi.org/10.1191/095968301678302940 http://journals.sagepub.com/doi/pdf/10.1191/095968301678302940 |
geographic |
Arctic Greenland Kola Peninsula |
geographic_facet |
Arctic Greenland Kola Peninsula |
genre |
Arctic Greenland Greenland Ice Sheet Project Ice Sheet kola peninsula |
genre_facet |
Arctic Greenland Greenland Ice Sheet Project Ice Sheet kola peninsula |
op_source |
The Holocene volume 11, issue 4, page 499-505 ISSN 0959-6836 1477-0911 |
op_rights |
http://journals.sagepub.com/page/policies/text-and-data-mining-license |
op_doi |
https://doi.org/10.1191/095968301678302940 |
container_title |
The Holocene |
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11 |
container_issue |
4 |
container_start_page |
499 |
op_container_end_page |
505 |
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1766335366821838848 |