Volcanic influence on centennial to millennial Holocene Greenland temperature change
Solar variability has been hypothesized to be a major driver of North Atlantic millennial-scale climate variations through the Holocene along with orbitally induced insolation change. However, another important climate driver, volcanic forcing has generally been underestimated prior to the past 2,50...
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ftunswworks:oai:unsworks.library.unsw.edu.au:1959.4/unsworks_53786 2024-05-12T08:04:12+00:00 Volcanic influence on centennial to millennial Holocene Greenland temperature change Kobashi, T Menviel, L Jeltsch-Thömmes, A Vinther, BM Box, JE Muscheler, R Nakaegawa, T Pfister, PL Döring, M Leuenberger, M Wanner, H Ohmura, A 2017-12-01 http://hdl.handle.net/1959.4/unsworks_53786 https://doi.org/10.1038/s41598-017-01451-7 unknown Springer Nature http://hdl.handle.net/1959.4/unsworks_53786 https://doi.org/10.1038/s41598-017-01451-7 open access https://purl.org/coar/access_right/c_abf2 CC BY https://creativecommons.org/licenses/by/4.0/ urn:ISSN:2045-2322 Scientific Reports, 7, 1, 1441 13 Climate Action journal article http://purl.org/coar/resource_type/c_6501 2017 ftunswworks https://doi.org/10.1038/s41598-017-01451-7 2024-04-17T15:21:40Z Solar variability has been hypothesized to be a major driver of North Atlantic millennial-scale climate variations through the Holocene along with orbitally induced insolation change. However, another important climate driver, volcanic forcing has generally been underestimated prior to the past 2,500 years partly owing to the lack of proper proxy temperature records. Here, we reconstruct seasonally unbiased and physically constrained Greenland Summit temperatures over the Holocene using argon and nitrogen isotopes within trapped air in a Greenland ice core (GISP2). We show that a series of volcanic eruptions through the Holocene played an important role in driving centennial to millennial-scale temperature changes in Greenland. The reconstructed Greenland temperature exhibits significant millennial correlations with K+ and Na+ ions in the GISP2 ice core (proxies for atmospheric circulation patterns), and δ18O of Oman and Chinese Dongge cave stalagmites (proxies for monsoon activity), indicating that the reconstructed temperature contains hemispheric signals. Climate model simulations forced with the volcanic forcing further suggest that a series of large volcanic eruptions induced hemispheric-wide centennial to millennial-scale variability through ocean/sea-ice feedbacks. Therefore, we conclude that volcanic activity played a critical role in driving centennial to millennial-scale Holocene temperature variability in Greenland and likely beyond. Article in Journal/Newspaper Greenland Greenland ice core ice core North Atlantic Sea ice UNSW Sydney (The University of New South Wales): UNSWorks Greenland Scientific Reports 7 1 |
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Open Polar |
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UNSW Sydney (The University of New South Wales): UNSWorks |
op_collection_id |
ftunswworks |
language |
unknown |
topic |
13 Climate Action |
spellingShingle |
13 Climate Action Kobashi, T Menviel, L Jeltsch-Thömmes, A Vinther, BM Box, JE Muscheler, R Nakaegawa, T Pfister, PL Döring, M Leuenberger, M Wanner, H Ohmura, A Volcanic influence on centennial to millennial Holocene Greenland temperature change |
topic_facet |
13 Climate Action |
description |
Solar variability has been hypothesized to be a major driver of North Atlantic millennial-scale climate variations through the Holocene along with orbitally induced insolation change. However, another important climate driver, volcanic forcing has generally been underestimated prior to the past 2,500 years partly owing to the lack of proper proxy temperature records. Here, we reconstruct seasonally unbiased and physically constrained Greenland Summit temperatures over the Holocene using argon and nitrogen isotopes within trapped air in a Greenland ice core (GISP2). We show that a series of volcanic eruptions through the Holocene played an important role in driving centennial to millennial-scale temperature changes in Greenland. The reconstructed Greenland temperature exhibits significant millennial correlations with K+ and Na+ ions in the GISP2 ice core (proxies for atmospheric circulation patterns), and δ18O of Oman and Chinese Dongge cave stalagmites (proxies for monsoon activity), indicating that the reconstructed temperature contains hemispheric signals. Climate model simulations forced with the volcanic forcing further suggest that a series of large volcanic eruptions induced hemispheric-wide centennial to millennial-scale variability through ocean/sea-ice feedbacks. Therefore, we conclude that volcanic activity played a critical role in driving centennial to millennial-scale Holocene temperature variability in Greenland and likely beyond. |
format |
Article in Journal/Newspaper |
author |
Kobashi, T Menviel, L Jeltsch-Thömmes, A Vinther, BM Box, JE Muscheler, R Nakaegawa, T Pfister, PL Döring, M Leuenberger, M Wanner, H Ohmura, A |
author_facet |
Kobashi, T Menviel, L Jeltsch-Thömmes, A Vinther, BM Box, JE Muscheler, R Nakaegawa, T Pfister, PL Döring, M Leuenberger, M Wanner, H Ohmura, A |
author_sort |
Kobashi, T |
title |
Volcanic influence on centennial to millennial Holocene Greenland temperature change |
title_short |
Volcanic influence on centennial to millennial Holocene Greenland temperature change |
title_full |
Volcanic influence on centennial to millennial Holocene Greenland temperature change |
title_fullStr |
Volcanic influence on centennial to millennial Holocene Greenland temperature change |
title_full_unstemmed |
Volcanic influence on centennial to millennial Holocene Greenland temperature change |
title_sort |
volcanic influence on centennial to millennial holocene greenland temperature change |
publisher |
Springer Nature |
publishDate |
2017 |
url |
http://hdl.handle.net/1959.4/unsworks_53786 https://doi.org/10.1038/s41598-017-01451-7 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Greenland ice core ice core North Atlantic Sea ice |
genre_facet |
Greenland Greenland ice core ice core North Atlantic Sea ice |
op_source |
urn:ISSN:2045-2322 Scientific Reports, 7, 1, 1441 |
op_relation |
http://hdl.handle.net/1959.4/unsworks_53786 https://doi.org/10.1038/s41598-017-01451-7 |
op_rights |
open access https://purl.org/coar/access_right/c_abf2 CC BY https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.1038/s41598-017-01451-7 |
container_title |
Scientific Reports |
container_volume |
7 |
container_issue |
1 |
_version_ |
1798846361194463232 |