Fire and ice : understanding volcanic histories from sulfur isotopes in ice cores ...
Reconstructing the history of explosive volcanic eruptions is important for understanding the frequency of eruptions and the climatic forcing of these events. Erupted volcanic SO₂ is oxidised to sulfate aerosols which scatter incoming solar radiation. Aerosols are then deposited at the poles resulti...
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ftdatacite:10.17630/sta/439 2023-07-23T04:19:47+02:00 Fire and ice : understanding volcanic histories from sulfur isotopes in ice cores ... Crick, Laura 2023 https://dx.doi.org/10.17630/sta/439 https://research-repository.st-andrews.ac.uk/handle/10023/27568 en eng The University of St Andrews Thesis restricted in accordance with University regulations. Restricted until 24th April 2028 2028-04-24 Creative Commons Attribution Non Commercial No Derivatives 4.0 International Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode cc-by-nc-nd-4.0 Volcanism Ice cores Sulfur isotopes Mass-independent fractionation Photochemical model QE522.C8 Sulfur--Isotopes Text article-journal ScholarlyArticle Thesis 2023 ftdatacite https://doi.org/10.17630/sta/439 2023-07-03T17:55:29Z Reconstructing the history of explosive volcanic eruptions is important for understanding the frequency of eruptions and the climatic forcing of these events. Erupted volcanic SO₂ is oxidised to sulfate aerosols which scatter incoming solar radiation. Aerosols are then deposited at the poles resulting in a peak in sulfate above background concentrations. Therefore, polar ice cores provide an important record of volcanism. The mass-independent fractionation of sulfur isotopes (S-MIF) in ice cores is an indicator of sulfur exposure to ultraviolet radiation via eruption into and above the ozone layer in the stratosphere. Sulfate aerosols from large eruptions that reach the stratosphere have a longer residence time and greater climatic impact than tropospheric aerosols from smaller eruptions. In this thesis I measure sulfur isotopes in volcanic ice core sulfate to investigate the ~74ka Toba supereruption and six unidentified volcanic eruptions from 16ka to 32ka. I found large magnitude S-MIF signals (-4.75‰) for ... Text ice core DataCite Metadata Store (German National Library of Science and Technology) |
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English |
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Volcanism Ice cores Sulfur isotopes Mass-independent fractionation Photochemical model QE522.C8 Sulfur--Isotopes |
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Volcanism Ice cores Sulfur isotopes Mass-independent fractionation Photochemical model QE522.C8 Sulfur--Isotopes Crick, Laura Fire and ice : understanding volcanic histories from sulfur isotopes in ice cores ... |
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Volcanism Ice cores Sulfur isotopes Mass-independent fractionation Photochemical model QE522.C8 Sulfur--Isotopes |
description |
Reconstructing the history of explosive volcanic eruptions is important for understanding the frequency of eruptions and the climatic forcing of these events. Erupted volcanic SO₂ is oxidised to sulfate aerosols which scatter incoming solar radiation. Aerosols are then deposited at the poles resulting in a peak in sulfate above background concentrations. Therefore, polar ice cores provide an important record of volcanism. The mass-independent fractionation of sulfur isotopes (S-MIF) in ice cores is an indicator of sulfur exposure to ultraviolet radiation via eruption into and above the ozone layer in the stratosphere. Sulfate aerosols from large eruptions that reach the stratosphere have a longer residence time and greater climatic impact than tropospheric aerosols from smaller eruptions. In this thesis I measure sulfur isotopes in volcanic ice core sulfate to investigate the ~74ka Toba supereruption and six unidentified volcanic eruptions from 16ka to 32ka. I found large magnitude S-MIF signals (-4.75‰) for ... |
format |
Text |
author |
Crick, Laura |
author_facet |
Crick, Laura |
author_sort |
Crick, Laura |
title |
Fire and ice : understanding volcanic histories from sulfur isotopes in ice cores ... |
title_short |
Fire and ice : understanding volcanic histories from sulfur isotopes in ice cores ... |
title_full |
Fire and ice : understanding volcanic histories from sulfur isotopes in ice cores ... |
title_fullStr |
Fire and ice : understanding volcanic histories from sulfur isotopes in ice cores ... |
title_full_unstemmed |
Fire and ice : understanding volcanic histories from sulfur isotopes in ice cores ... |
title_sort |
fire and ice : understanding volcanic histories from sulfur isotopes in ice cores ... |
publisher |
The University of St Andrews |
publishDate |
2023 |
url |
https://dx.doi.org/10.17630/sta/439 https://research-repository.st-andrews.ac.uk/handle/10023/27568 |
genre |
ice core |
genre_facet |
ice core |
op_rights |
Thesis restricted in accordance with University regulations. Restricted until 24th April 2028 2028-04-24 Creative Commons Attribution Non Commercial No Derivatives 4.0 International Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode cc-by-nc-nd-4.0 |
op_doi |
https://doi.org/10.17630/sta/439 |
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1772183177178120192 |