A 4500-Year Tree-Ring Record of Extreme Climatic Events on the Yamal Peninsula
Based on the analysis of the frequency of anomalous anatomical structures in the wood of Siberian larch and Siberian spruce (frost rings, light rings, and false rings, as well as missing and narrow rings), we reconstructed a timeline of climatic extremes (summer frosts, sharp multiday decreases in a...
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ftmdpi:oai:mdpi.com:/1999-4907/14/3/574/ 2023-08-20T04:01:12+02:00 A 4500-Year Tree-Ring Record of Extreme Climatic Events on the Yamal Peninsula Rashit Hantemirov Liudmila Gorlanova Varvara Bessonova Ildar Hamzin Vladimir Kukarskih agris 2023-03-14 application/pdf https://doi.org/10.3390/f14030574 EN eng Multidisciplinary Digital Publishing Institute Forest Meteorology and Climate Change https://dx.doi.org/10.3390/f14030574 https://creativecommons.org/licenses/by/4.0/ Forests; Volume 14; Issue 3; Pages: 574 Yamal tree rings anomalous structures Holocene Larix sibirica reconstruction Text 2023 ftmdpi https://doi.org/10.3390/f14030574 2023-08-01T09:15:28Z Based on the analysis of the frequency of anomalous anatomical structures in the wood of Siberian larch and Siberian spruce (frost rings, light rings, and false rings, as well as missing and narrow rings), we reconstructed a timeline of climatic extremes (summer frosts, sharp multiday decreases in air temperature during the growing season, and low average summer temperatures) in Yamal (Western Siberia) over the last 4500 years. In total, 229 years were determined to have experienced extreme events. The most significant temperature extremes were recorded in 2053, 1935, 1647, 1626, 1553, 1538, 1410, 1401, 982, 919, 883 BCE, 143, 404, 543, 640, 1209, 1440, 1453, 1466, 1481, 1601 and 1818 CE. These dates with extrema observed in Yamal corrobarated with tree ring data from other regions and revealed several coincidences. That is, in these years, the observed extremes appeared to have been on a global rather than a regional scale. Moreover, these dates coincided with traces of large volcanic eruptions found in ice cores from Greenland and Antarctica, dated to approximately the same years. Therefore, the cause of the extreme summer cooling on a global scale, in most cases, can be linked to large volcanic eruptions. Text Antarc* Antarctica Greenland Yamal Peninsula Siberia MDPI Open Access Publishing Greenland Yamal Peninsula ENVELOPE(69.873,69.873,70.816,70.816) Forests 14 3 574 |
institution |
Open Polar |
collection |
MDPI Open Access Publishing |
op_collection_id |
ftmdpi |
language |
English |
topic |
Yamal tree rings anomalous structures Holocene Larix sibirica reconstruction |
spellingShingle |
Yamal tree rings anomalous structures Holocene Larix sibirica reconstruction Rashit Hantemirov Liudmila Gorlanova Varvara Bessonova Ildar Hamzin Vladimir Kukarskih A 4500-Year Tree-Ring Record of Extreme Climatic Events on the Yamal Peninsula |
topic_facet |
Yamal tree rings anomalous structures Holocene Larix sibirica reconstruction |
description |
Based on the analysis of the frequency of anomalous anatomical structures in the wood of Siberian larch and Siberian spruce (frost rings, light rings, and false rings, as well as missing and narrow rings), we reconstructed a timeline of climatic extremes (summer frosts, sharp multiday decreases in air temperature during the growing season, and low average summer temperatures) in Yamal (Western Siberia) over the last 4500 years. In total, 229 years were determined to have experienced extreme events. The most significant temperature extremes were recorded in 2053, 1935, 1647, 1626, 1553, 1538, 1410, 1401, 982, 919, 883 BCE, 143, 404, 543, 640, 1209, 1440, 1453, 1466, 1481, 1601 and 1818 CE. These dates with extrema observed in Yamal corrobarated with tree ring data from other regions and revealed several coincidences. That is, in these years, the observed extremes appeared to have been on a global rather than a regional scale. Moreover, these dates coincided with traces of large volcanic eruptions found in ice cores from Greenland and Antarctica, dated to approximately the same years. Therefore, the cause of the extreme summer cooling on a global scale, in most cases, can be linked to large volcanic eruptions. |
format |
Text |
author |
Rashit Hantemirov Liudmila Gorlanova Varvara Bessonova Ildar Hamzin Vladimir Kukarskih |
author_facet |
Rashit Hantemirov Liudmila Gorlanova Varvara Bessonova Ildar Hamzin Vladimir Kukarskih |
author_sort |
Rashit Hantemirov |
title |
A 4500-Year Tree-Ring Record of Extreme Climatic Events on the Yamal Peninsula |
title_short |
A 4500-Year Tree-Ring Record of Extreme Climatic Events on the Yamal Peninsula |
title_full |
A 4500-Year Tree-Ring Record of Extreme Climatic Events on the Yamal Peninsula |
title_fullStr |
A 4500-Year Tree-Ring Record of Extreme Climatic Events on the Yamal Peninsula |
title_full_unstemmed |
A 4500-Year Tree-Ring Record of Extreme Climatic Events on the Yamal Peninsula |
title_sort |
4500-year tree-ring record of extreme climatic events on the yamal peninsula |
publisher |
Multidisciplinary Digital Publishing Institute |
publishDate |
2023 |
url |
https://doi.org/10.3390/f14030574 |
op_coverage |
agris |
long_lat |
ENVELOPE(69.873,69.873,70.816,70.816) |
geographic |
Greenland Yamal Peninsula |
geographic_facet |
Greenland Yamal Peninsula |
genre |
Antarc* Antarctica Greenland Yamal Peninsula Siberia |
genre_facet |
Antarc* Antarctica Greenland Yamal Peninsula Siberia |
op_source |
Forests; Volume 14; Issue 3; Pages: 574 |
op_relation |
Forest Meteorology and Climate Change https://dx.doi.org/10.3390/f14030574 |
op_rights |
https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.3390/f14030574 |
container_title |
Forests |
container_volume |
14 |
container_issue |
3 |
container_start_page |
574 |
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1774723447271718912 |