Satellite-derived sulfur dioxide (SO 2 ) emissions from the 2014–2015 Holuhraun eruption (Iceland)
The 6-month-long 2014–2015 Holuhraun eruption was the largest in Iceland for 200 years, emitting huge quantities of sulfur dioxide ( SO 2 ) into the troposphere, at times overwhelming European anthropogenic emissions. Weather, terrain and latitude made continuous ground-based or UV satellite sensor...
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ftdoajarticles:oai:doaj.org/article:dfbf2a0eb57e4de8a6bc1cb811063cfa 2023-05-15T16:49:39+02:00 Satellite-derived sulfur dioxide (SO 2 ) emissions from the 2014–2015 Holuhraun eruption (Iceland) E. Carboni T. A. Mather A. Schmidt R. G. Grainger M. A. Pfeffer I. Ialongo N. Theys 2019-04-01T00:00:00Z https://doi.org/10.5194/acp-19-4851-2019 https://doaj.org/article/dfbf2a0eb57e4de8a6bc1cb811063cfa EN eng Copernicus Publications https://www.atmos-chem-phys.net/19/4851/2019/acp-19-4851-2019.pdf https://doaj.org/toc/1680-7316 https://doaj.org/toc/1680-7324 doi:10.5194/acp-19-4851-2019 1680-7316 1680-7324 https://doaj.org/article/dfbf2a0eb57e4de8a6bc1cb811063cfa Atmospheric Chemistry and Physics, Vol 19, Pp 4851-4862 (2019) Physics QC1-999 Chemistry QD1-999 article 2019 ftdoajarticles https://doi.org/10.5194/acp-19-4851-2019 2022-12-30T21:12:55Z The 6-month-long 2014–2015 Holuhraun eruption was the largest in Iceland for 200 years, emitting huge quantities of sulfur dioxide ( SO 2 ) into the troposphere, at times overwhelming European anthropogenic emissions. Weather, terrain and latitude made continuous ground-based or UV satellite sensor measurements challenging. Infrared Atmospheric Sounding Interferometer (IASI) data are used to derive the first time series of daily SO 2 mass present in the atmosphere and its vertical distribution over the entire eruption period. A new optimal estimation scheme is used to calculate daily SO 2 fluxes and average e -folding time every 12 h. For the 6 months studied, the SO 2 flux was observed to be up to 200 kt day −1 and the minimum total SO 2 erupted mass was 4.4±0.8 Tg. The average SO 2 e -folding time was 2.4±0.6 days. Where comparisons are possible, these results broadly agree with ground-based near-source measurements, independent remote-sensing data and values obtained from model simulations from a previous paper. The results highlight the importance of using high-resolution time series data to accurately estimate volcanic SO 2 emissions. The SO 2 mass missed due to thermal contrast is estimated to be of the order of 3 % of the total emission when compared to measurements by the Ozone Monitoring Instrument. A statistical correction for cloud based on the AVHRR cloud-CCI data set suggested that the SO 2 mass missed due to cloud cover could be significant, up to a factor of 2 for the plume within the first kilometre from the vent. Applying this correction results in a total erupted mass of 6.7±0.4 Tg and little change in average e -folding time. The data set derived can be used for comparisons to other ground- and satellite-based measurements and to petrological estimates of the SO 2 flux. It could also be used to initialise climate model simulations, helping to better quantify the environmental and climatic impacts of future Icelandic fissure eruptions and simulations of past large-scale flood lava eruptions. Article in Journal/Newspaper Iceland Directory of Open Access Journals: DOAJ Articles Holuhraun ENVELOPE(-16.831,-16.831,64.852,64.852) Atmospheric Chemistry and Physics 19 7 4851 4862 |
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Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Physics QC1-999 Chemistry QD1-999 |
spellingShingle |
Physics QC1-999 Chemistry QD1-999 E. Carboni T. A. Mather A. Schmidt R. G. Grainger M. A. Pfeffer I. Ialongo N. Theys Satellite-derived sulfur dioxide (SO 2 ) emissions from the 2014–2015 Holuhraun eruption (Iceland) |
topic_facet |
Physics QC1-999 Chemistry QD1-999 |
description |
The 6-month-long 2014–2015 Holuhraun eruption was the largest in Iceland for 200 years, emitting huge quantities of sulfur dioxide ( SO 2 ) into the troposphere, at times overwhelming European anthropogenic emissions. Weather, terrain and latitude made continuous ground-based or UV satellite sensor measurements challenging. Infrared Atmospheric Sounding Interferometer (IASI) data are used to derive the first time series of daily SO 2 mass present in the atmosphere and its vertical distribution over the entire eruption period. A new optimal estimation scheme is used to calculate daily SO 2 fluxes and average e -folding time every 12 h. For the 6 months studied, the SO 2 flux was observed to be up to 200 kt day −1 and the minimum total SO 2 erupted mass was 4.4±0.8 Tg. The average SO 2 e -folding time was 2.4±0.6 days. Where comparisons are possible, these results broadly agree with ground-based near-source measurements, independent remote-sensing data and values obtained from model simulations from a previous paper. The results highlight the importance of using high-resolution time series data to accurately estimate volcanic SO 2 emissions. The SO 2 mass missed due to thermal contrast is estimated to be of the order of 3 % of the total emission when compared to measurements by the Ozone Monitoring Instrument. A statistical correction for cloud based on the AVHRR cloud-CCI data set suggested that the SO 2 mass missed due to cloud cover could be significant, up to a factor of 2 for the plume within the first kilometre from the vent. Applying this correction results in a total erupted mass of 6.7±0.4 Tg and little change in average e -folding time. The data set derived can be used for comparisons to other ground- and satellite-based measurements and to petrological estimates of the SO 2 flux. It could also be used to initialise climate model simulations, helping to better quantify the environmental and climatic impacts of future Icelandic fissure eruptions and simulations of past large-scale flood lava eruptions. |
format |
Article in Journal/Newspaper |
author |
E. Carboni T. A. Mather A. Schmidt R. G. Grainger M. A. Pfeffer I. Ialongo N. Theys |
author_facet |
E. Carboni T. A. Mather A. Schmidt R. G. Grainger M. A. Pfeffer I. Ialongo N. Theys |
author_sort |
E. Carboni |
title |
Satellite-derived sulfur dioxide (SO 2 ) emissions from the 2014–2015 Holuhraun eruption (Iceland) |
title_short |
Satellite-derived sulfur dioxide (SO 2 ) emissions from the 2014–2015 Holuhraun eruption (Iceland) |
title_full |
Satellite-derived sulfur dioxide (SO 2 ) emissions from the 2014–2015 Holuhraun eruption (Iceland) |
title_fullStr |
Satellite-derived sulfur dioxide (SO 2 ) emissions from the 2014–2015 Holuhraun eruption (Iceland) |
title_full_unstemmed |
Satellite-derived sulfur dioxide (SO 2 ) emissions from the 2014–2015 Holuhraun eruption (Iceland) |
title_sort |
satellite-derived sulfur dioxide (so 2 ) emissions from the 2014–2015 holuhraun eruption (iceland) |
publisher |
Copernicus Publications |
publishDate |
2019 |
url |
https://doi.org/10.5194/acp-19-4851-2019 https://doaj.org/article/dfbf2a0eb57e4de8a6bc1cb811063cfa |
long_lat |
ENVELOPE(-16.831,-16.831,64.852,64.852) |
geographic |
Holuhraun |
geographic_facet |
Holuhraun |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
Atmospheric Chemistry and Physics, Vol 19, Pp 4851-4862 (2019) |
op_relation |
https://www.atmos-chem-phys.net/19/4851/2019/acp-19-4851-2019.pdf https://doaj.org/toc/1680-7316 https://doaj.org/toc/1680-7324 doi:10.5194/acp-19-4851-2019 1680-7316 1680-7324 https://doaj.org/article/dfbf2a0eb57e4de8a6bc1cb811063cfa |
op_doi |
https://doi.org/10.5194/acp-19-4851-2019 |
container_title |
Atmospheric Chemistry and Physics |
container_volume |
19 |
container_issue |
7 |
container_start_page |
4851 |
op_container_end_page |
4862 |
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1766039781876170752 |