The Role of Small to Moderate Volcanic Eruptions in the Early 19th Century Climate

Small-to-moderate volcanic eruptions can lead to significant surface cooling when they occur clustered, as observed in recent decades. In this study, based on new high-resolution ice-core data from Greenland, we produce a new volcanic forcing data set that includes several small-to-moderate eruption...

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Published in:Geophysical Research Letters
Main Authors: Fang S. -W., Sigl M., Toohey M., Jungclaus J., Zanchettin D., Timmreck C.
Other Authors: Fang, S. -W., Sigl, M., Toohey, M., Jungclaus, J., Zanchettin, D., Timmreck, C.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2023
Subjects:
Online Access:https://hdl.handle.net/10278/5044528
https://doi.org/10.1029/2023GL105307
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spelling ftuniveneziairis:oai:iris.unive.it:10278/5044528 2024-04-14T08:12:31+00:00 The Role of Small to Moderate Volcanic Eruptions in the Early 19th Century Climate Fang S. -W. Sigl M. Toohey M. Jungclaus J. Zanchettin D. Timmreck C. Fang, S. -W. Sigl, M. Toohey, M. Jungclaus, J. Zanchettin, D. Timmreck, C. 2023 https://hdl.handle.net/10278/5044528 https://doi.org/10.1029/2023GL105307 unknown volume:50 issue:22 journal:GEOPHYSICAL RESEARCH LETTERS https://hdl.handle.net/10278/5044528 doi:10.1029/2023GL105307 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85177672338 info:eu-repo/semantics/openAccess early 19th century ice-core data small eruption Tambora eruption volcanic reconstruction volcano impact Settore GEO/12 - Oceanografia e Fisica dell'Atmosfera info:eu-repo/semantics/article 2023 ftuniveneziairis https://doi.org/10.1029/2023GL105307 2024-03-21T17:57:10Z Small-to-moderate volcanic eruptions can lead to significant surface cooling when they occur clustered, as observed in recent decades. In this study, based on new high-resolution ice-core data from Greenland, we produce a new volcanic forcing data set that includes several small-to-moderate eruptions not included in prior reconstructions and investigate their climate impacts of the early 19th century through ensemble simulations with the Max Planck Institute Earth System Model. We find that clustered small-to-moderate eruptions produce significant additional global surface cooling (∼0.07 K) during the period 1812–1820, superposing with the cooling by large eruptions in 1809 (unidentified location) and 1815 (Tambora). This additional cooling helps explain the reconstructed long-lasting cooling after the large eruptions, but simulated regional impacts cannot be confirmed with reconstructions due to a low signal-to-noise ratio. This study highlights the importance of small-to-moderate eruptions for climate simulations as their impacts can be comparable with that of solar irradiance changes. Article in Journal/Newspaper Greenland ice core Università Ca’ Foscari Venezia: ARCA (Archivio Istituzionale della Ricerca) Greenland Geophysical Research Letters 50 22
institution Open Polar
collection Università Ca’ Foscari Venezia: ARCA (Archivio Istituzionale della Ricerca)
op_collection_id ftuniveneziairis
language unknown
topic early 19th century
ice-core data
small eruption
Tambora eruption
volcanic reconstruction
volcano impact
Settore GEO/12 - Oceanografia e Fisica dell'Atmosfera
spellingShingle early 19th century
ice-core data
small eruption
Tambora eruption
volcanic reconstruction
volcano impact
Settore GEO/12 - Oceanografia e Fisica dell'Atmosfera
Fang S. -W.
Sigl M.
Toohey M.
Jungclaus J.
Zanchettin D.
Timmreck C.
The Role of Small to Moderate Volcanic Eruptions in the Early 19th Century Climate
topic_facet early 19th century
ice-core data
small eruption
Tambora eruption
volcanic reconstruction
volcano impact
Settore GEO/12 - Oceanografia e Fisica dell'Atmosfera
description Small-to-moderate volcanic eruptions can lead to significant surface cooling when they occur clustered, as observed in recent decades. In this study, based on new high-resolution ice-core data from Greenland, we produce a new volcanic forcing data set that includes several small-to-moderate eruptions not included in prior reconstructions and investigate their climate impacts of the early 19th century through ensemble simulations with the Max Planck Institute Earth System Model. We find that clustered small-to-moderate eruptions produce significant additional global surface cooling (∼0.07 K) during the period 1812–1820, superposing with the cooling by large eruptions in 1809 (unidentified location) and 1815 (Tambora). This additional cooling helps explain the reconstructed long-lasting cooling after the large eruptions, but simulated regional impacts cannot be confirmed with reconstructions due to a low signal-to-noise ratio. This study highlights the importance of small-to-moderate eruptions for climate simulations as their impacts can be comparable with that of solar irradiance changes.
author2 Fang, S. -W.
Sigl, M.
Toohey, M.
Jungclaus, J.
Zanchettin, D.
Timmreck, C.
format Article in Journal/Newspaper
author Fang S. -W.
Sigl M.
Toohey M.
Jungclaus J.
Zanchettin D.
Timmreck C.
author_facet Fang S. -W.
Sigl M.
Toohey M.
Jungclaus J.
Zanchettin D.
Timmreck C.
author_sort Fang S. -W.
title The Role of Small to Moderate Volcanic Eruptions in the Early 19th Century Climate
title_short The Role of Small to Moderate Volcanic Eruptions in the Early 19th Century Climate
title_full The Role of Small to Moderate Volcanic Eruptions in the Early 19th Century Climate
title_fullStr The Role of Small to Moderate Volcanic Eruptions in the Early 19th Century Climate
title_full_unstemmed The Role of Small to Moderate Volcanic Eruptions in the Early 19th Century Climate
title_sort role of small to moderate volcanic eruptions in the early 19th century climate
publishDate 2023
url https://hdl.handle.net/10278/5044528
https://doi.org/10.1029/2023GL105307
geographic Greenland
geographic_facet Greenland
genre Greenland
ice core
genre_facet Greenland
ice core
op_relation volume:50
issue:22
journal:GEOPHYSICAL RESEARCH LETTERS
https://hdl.handle.net/10278/5044528
doi:10.1029/2023GL105307
info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85177672338
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1029/2023GL105307
container_title Geophysical Research Letters
container_volume 50
container_issue 22
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