Evaluating the structure and magnitude of the ash plume during the initial phase of the 2010 Eyjafjallajokull eruption using lidar observations and NAME simulations

The Eyjafjallajokull volcano in Iceland erupted explosively on 14 April 2010, emitting a plume of ash into the atmosphere. The ash was transported from Iceland toward Europe where mostly cloud-free skies allowed ground-based lidars at Chilbolton in England and Leipzig in Germany to estimate the mass...

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Published in:Journal of Geophysical Research
Main Authors: Dacre, H., Grant, A., Hogan, R., Belcher, S., Thomson, D., Devenish, B., Marenco, F., Hort, M., Haywood, J., Ansmann, A., Mattis, I., Clarisse, L.
Format: Article in Journal/Newspaper
Language:English
Published: 2011
Subjects:
Online Access:http://hdl.handle.net/11858/00-001M-0000-0018-10B4-4
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spelling ftpubman:oai:pure.mpg.de:item_1920739 2024-09-15T18:13:37+00:00 Evaluating the structure and magnitude of the ash plume during the initial phase of the 2010 Eyjafjallajokull eruption using lidar observations and NAME simulations Dacre, H. Grant, A. Hogan, R. Belcher, S. Thomson, D. Devenish, B. Marenco, F. Hort, M. Haywood, J. Ansmann, A. Mattis, I. Clarisse, L. 2011 http://hdl.handle.net/11858/00-001M-0000-0018-10B4-4 eng eng info:eu-repo/semantics/altIdentifier/doi/10.1029/2011JD015608 http://hdl.handle.net/11858/00-001M-0000-0018-10B4-4 JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES info:eu-repo/semantics/article 2011 ftpubman https://doi.org/10.1029/2011JD015608 2024-07-31T09:31:25Z The Eyjafjallajokull volcano in Iceland erupted explosively on 14 April 2010, emitting a plume of ash into the atmosphere. The ash was transported from Iceland toward Europe where mostly cloud-free skies allowed ground-based lidars at Chilbolton in England and Leipzig in Germany to estimate the mass concentration in the ash cloud as it passed overhead. The UK Met Office's Numerical Atmospheric-dispersion Modeling Environment (NAME) has been used to simulate the evolution of the ash cloud from the Eyjafjallajokull volcano during the initial phase of the ash emissions, 14-16 April 2010. NAME captures the timing and sloped structure of the ash layer observed over Leipzig, close to the central axis of the ash cloud. Relatively small errors in the ash cloud position, probably caused by the cumulative effect of errors in the driving meteorology en route, result in a timing error at distances far from the central axis of the ash cloud. Taking the timing error into account, NAME is able to capture the sloped ash layer over the UK. Comparison of the lidar observations and NAME simulations has allowed an estimation of the plume height time series to be made. It is necessary to include in the model input the large variations in plume height in order to accurately predict the ash cloud structure at long range. Quantitative comparison with the mass concentrations at Leipzig and Chilbolton suggest that around 3% of the total emitted mass is transported as far as these sites by small (<100 mu m diameter) ash particles. Article in Journal/Newspaper Iceland Max Planck Society: MPG.PuRe Journal of Geophysical Research 116
institution Open Polar
collection Max Planck Society: MPG.PuRe
op_collection_id ftpubman
language English
description The Eyjafjallajokull volcano in Iceland erupted explosively on 14 April 2010, emitting a plume of ash into the atmosphere. The ash was transported from Iceland toward Europe where mostly cloud-free skies allowed ground-based lidars at Chilbolton in England and Leipzig in Germany to estimate the mass concentration in the ash cloud as it passed overhead. The UK Met Office's Numerical Atmospheric-dispersion Modeling Environment (NAME) has been used to simulate the evolution of the ash cloud from the Eyjafjallajokull volcano during the initial phase of the ash emissions, 14-16 April 2010. NAME captures the timing and sloped structure of the ash layer observed over Leipzig, close to the central axis of the ash cloud. Relatively small errors in the ash cloud position, probably caused by the cumulative effect of errors in the driving meteorology en route, result in a timing error at distances far from the central axis of the ash cloud. Taking the timing error into account, NAME is able to capture the sloped ash layer over the UK. Comparison of the lidar observations and NAME simulations has allowed an estimation of the plume height time series to be made. It is necessary to include in the model input the large variations in plume height in order to accurately predict the ash cloud structure at long range. Quantitative comparison with the mass concentrations at Leipzig and Chilbolton suggest that around 3% of the total emitted mass is transported as far as these sites by small (<100 mu m diameter) ash particles.
format Article in Journal/Newspaper
author Dacre, H.
Grant, A.
Hogan, R.
Belcher, S.
Thomson, D.
Devenish, B.
Marenco, F.
Hort, M.
Haywood, J.
Ansmann, A.
Mattis, I.
Clarisse, L.
spellingShingle Dacre, H.
Grant, A.
Hogan, R.
Belcher, S.
Thomson, D.
Devenish, B.
Marenco, F.
Hort, M.
Haywood, J.
Ansmann, A.
Mattis, I.
Clarisse, L.
Evaluating the structure and magnitude of the ash plume during the initial phase of the 2010 Eyjafjallajokull eruption using lidar observations and NAME simulations
author_facet Dacre, H.
Grant, A.
Hogan, R.
Belcher, S.
Thomson, D.
Devenish, B.
Marenco, F.
Hort, M.
Haywood, J.
Ansmann, A.
Mattis, I.
Clarisse, L.
author_sort Dacre, H.
title Evaluating the structure and magnitude of the ash plume during the initial phase of the 2010 Eyjafjallajokull eruption using lidar observations and NAME simulations
title_short Evaluating the structure and magnitude of the ash plume during the initial phase of the 2010 Eyjafjallajokull eruption using lidar observations and NAME simulations
title_full Evaluating the structure and magnitude of the ash plume during the initial phase of the 2010 Eyjafjallajokull eruption using lidar observations and NAME simulations
title_fullStr Evaluating the structure and magnitude of the ash plume during the initial phase of the 2010 Eyjafjallajokull eruption using lidar observations and NAME simulations
title_full_unstemmed Evaluating the structure and magnitude of the ash plume during the initial phase of the 2010 Eyjafjallajokull eruption using lidar observations and NAME simulations
title_sort evaluating the structure and magnitude of the ash plume during the initial phase of the 2010 eyjafjallajokull eruption using lidar observations and name simulations
publishDate 2011
url http://hdl.handle.net/11858/00-001M-0000-0018-10B4-4
genre Iceland
genre_facet Iceland
op_source JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1029/2011JD015608
http://hdl.handle.net/11858/00-001M-0000-0018-10B4-4
op_doi https://doi.org/10.1029/2011JD015608
container_title Journal of Geophysical Research
container_volume 116
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