UK monitoring and deposition of tephra from the May 2011 eruption of Grímsvötn, Iceland.
Mapping the transport and deposition of tephra is important for the assessment of an eruption’s impact on health, transport, vegetation and infrastructure, but it is challenging at large distances from a volcano (> 1000 km), where it may not be visible to the naked eye. Here we describe a range o...
Published in: | Journal of Applied Volcanology |
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Online Access: | http://dro.dur.ac.uk/16408/ http://dro.dur.ac.uk/16408/1/16408.pdf https://doi.org/10.1186/2191-5040-2-3 |
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ftunivdurham:oai:dro.dur.ac.uk.OAI2:16408 2023-05-15T16:50:02+02:00 UK monitoring and deposition of tephra from the May 2011 eruption of Grímsvötn, Iceland. Stevenson, J.A. Loughlin, S.C. Font, A. Fuller, G.W. MacLeod, A. Oliver, I.W. Jackson, B. Horwell, C.J. Thordarson, T. Dawson, I. 2013-05-24 application/pdf http://dro.dur.ac.uk/16408/ http://dro.dur.ac.uk/16408/1/16408.pdf https://doi.org/10.1186/2191-5040-2-3 unknown Springer dro:16408 issn:2191-5040 doi:10.1186/2191-5040-2-3 http://dro.dur.ac.uk/16408/ http://dx.doi.org/10.1186/2191-5040-2-3 http://dro.dur.ac.uk/16408/1/16408.pdf © 2013 Stevenson et al.; licensee Springer. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/2.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. CC-BY Journal of applied volcanology, 2013, Vol.2(1), pp.3 [Peer Reviewed Journal] Tephrochronology Volcanic ash PM10 PM 2.5 Citizen science Article PeerReviewed 2013 ftunivdurham https://doi.org/10.1186/2191-5040-2-3 2020-05-28T22:33:14Z Mapping the transport and deposition of tephra is important for the assessment of an eruption’s impact on health, transport, vegetation and infrastructure, but it is challenging at large distances from a volcano (> 1000 km), where it may not be visible to the naked eye. Here we describe a range of methods used to quantify tephra deposition and impact on air quality during the 21–28 May 2011 explosive basaltic eruption of Grímsvötn volcano, Iceland. Tephra was detected in the UK with tape-on-paper samples, rainwater samples, rainwater chemistry analysis, pollen slides and air quality measurements. Combined results show that deposition was mainly in Scotland, on 23–25 May. Deposition was patchy, with adjacent locations recording different results. Tape-on-paper samples, collected by volunteer citizen scientists, and giving excellent coverage across the UK, showed deposition at latitudes >55°N, mainly on 24 May. Rainwater samples contained ash grains mostly 20–30 μm long (maximum recorded grainsize 80 μm) with loadings of up to 116 grainscm-2. Analysis of rainwater chemistry showed high concentrations of dissolved Fe and Al in samples from N Scotland on 24–27 May. Pollen slides recorded small glass shards (3–4 μm long) deposited during rainfall on 24–25 May and again on 27 May. Air quality monitoring detected increased particulate matter concentrations in many parts of the country. An hourly concentration of particles < 10 μm in diameter (PM10) of ∼413 μgm-3, was measured in Aberdeen at 02:00hrs on 24 May 2011. Significant peaks of non-anthropogenic PM, which is most likely to have a volcanic origin, could be tracked as far south as the English Midlands (> 53°N) on 24 May but no negative effects on health were reported. Although the eruption column reached altitudes of 20 km above sea level, air mass trajectories suggest that only tephra from the lowest 4 km above sea level of the eruption plume was transported to the UK. This demonstrates that even low plumes could deliver tephra to the UK and suggests that the relative lack of basaltic tephra in the tephrochronological record is not due to transport processes. Article in Journal/Newspaper Iceland Durham University: Durham Research Online Journal of Applied Volcanology 2 1 |
institution |
Open Polar |
collection |
Durham University: Durham Research Online |
op_collection_id |
ftunivdurham |
language |
unknown |
topic |
Tephrochronology Volcanic ash PM10 PM 2.5 Citizen science |
spellingShingle |
Tephrochronology Volcanic ash PM10 PM 2.5 Citizen science Stevenson, J.A. Loughlin, S.C. Font, A. Fuller, G.W. MacLeod, A. Oliver, I.W. Jackson, B. Horwell, C.J. Thordarson, T. Dawson, I. UK monitoring and deposition of tephra from the May 2011 eruption of Grímsvötn, Iceland. |
topic_facet |
Tephrochronology Volcanic ash PM10 PM 2.5 Citizen science |
description |
Mapping the transport and deposition of tephra is important for the assessment of an eruption’s impact on health, transport, vegetation and infrastructure, but it is challenging at large distances from a volcano (> 1000 km), where it may not be visible to the naked eye. Here we describe a range of methods used to quantify tephra deposition and impact on air quality during the 21–28 May 2011 explosive basaltic eruption of Grímsvötn volcano, Iceland. Tephra was detected in the UK with tape-on-paper samples, rainwater samples, rainwater chemistry analysis, pollen slides and air quality measurements. Combined results show that deposition was mainly in Scotland, on 23–25 May. Deposition was patchy, with adjacent locations recording different results. Tape-on-paper samples, collected by volunteer citizen scientists, and giving excellent coverage across the UK, showed deposition at latitudes >55°N, mainly on 24 May. Rainwater samples contained ash grains mostly 20–30 μm long (maximum recorded grainsize 80 μm) with loadings of up to 116 grainscm-2. Analysis of rainwater chemistry showed high concentrations of dissolved Fe and Al in samples from N Scotland on 24–27 May. Pollen slides recorded small glass shards (3–4 μm long) deposited during rainfall on 24–25 May and again on 27 May. Air quality monitoring detected increased particulate matter concentrations in many parts of the country. An hourly concentration of particles < 10 μm in diameter (PM10) of ∼413 μgm-3, was measured in Aberdeen at 02:00hrs on 24 May 2011. Significant peaks of non-anthropogenic PM, which is most likely to have a volcanic origin, could be tracked as far south as the English Midlands (> 53°N) on 24 May but no negative effects on health were reported. Although the eruption column reached altitudes of 20 km above sea level, air mass trajectories suggest that only tephra from the lowest 4 km above sea level of the eruption plume was transported to the UK. This demonstrates that even low plumes could deliver tephra to the UK and suggests that the relative lack of basaltic tephra in the tephrochronological record is not due to transport processes. |
format |
Article in Journal/Newspaper |
author |
Stevenson, J.A. Loughlin, S.C. Font, A. Fuller, G.W. MacLeod, A. Oliver, I.W. Jackson, B. Horwell, C.J. Thordarson, T. Dawson, I. |
author_facet |
Stevenson, J.A. Loughlin, S.C. Font, A. Fuller, G.W. MacLeod, A. Oliver, I.W. Jackson, B. Horwell, C.J. Thordarson, T. Dawson, I. |
author_sort |
Stevenson, J.A. |
title |
UK monitoring and deposition of tephra from the May 2011 eruption of Grímsvötn, Iceland. |
title_short |
UK monitoring and deposition of tephra from the May 2011 eruption of Grímsvötn, Iceland. |
title_full |
UK monitoring and deposition of tephra from the May 2011 eruption of Grímsvötn, Iceland. |
title_fullStr |
UK monitoring and deposition of tephra from the May 2011 eruption of Grímsvötn, Iceland. |
title_full_unstemmed |
UK monitoring and deposition of tephra from the May 2011 eruption of Grímsvötn, Iceland. |
title_sort |
uk monitoring and deposition of tephra from the may 2011 eruption of grímsvötn, iceland. |
publisher |
Springer |
publishDate |
2013 |
url |
http://dro.dur.ac.uk/16408/ http://dro.dur.ac.uk/16408/1/16408.pdf https://doi.org/10.1186/2191-5040-2-3 |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
Journal of applied volcanology, 2013, Vol.2(1), pp.3 [Peer Reviewed Journal] |
op_relation |
dro:16408 issn:2191-5040 doi:10.1186/2191-5040-2-3 http://dro.dur.ac.uk/16408/ http://dx.doi.org/10.1186/2191-5040-2-3 http://dro.dur.ac.uk/16408/1/16408.pdf |
op_rights |
© 2013 Stevenson et al.; licensee Springer. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/2.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1186/2191-5040-2-3 |
container_title |
Journal of Applied Volcanology |
container_volume |
2 |
container_issue |
1 |
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1766040215682547712 |