Inferring the size distribution of volcanic ash from IASI measurements and optimal estimation

This study demonstrates a method of retrieving the mass column loading and cloud-top pressure of a volcanic ash cloud, together with the effective radius and spread of the ash particle size distribution, as well as the cloud top pressure of any underlying water cloud, using an optimal estimation tec...

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Main Authors: Western, Luke M., Francis, Peter N., Watson, I. Matthew, Mackie, Shona
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/amt-2016-92
https://amt.copernicus.org/preprints/amt-2016-92/
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spelling ftcopernicus:oai:publications.copernicus.org:amtd50380 2023-05-15T16:50:43+02:00 Inferring the size distribution of volcanic ash from IASI measurements and optimal estimation Western, Luke M. Francis, Peter N. Watson, I. Matthew Mackie, Shona 2018-08-10 application/pdf https://doi.org/10.5194/amt-2016-92 https://amt.copernicus.org/preprints/amt-2016-92/ eng eng doi:10.5194/amt-2016-92 https://amt.copernicus.org/preprints/amt-2016-92/ eISSN: 1867-8548 Text 2018 ftcopernicus https://doi.org/10.5194/amt-2016-92 2020-07-20T16:24:09Z This study demonstrates a method of retrieving the mass column loading and cloud-top pressure of a volcanic ash cloud, together with the effective radius and spread of the ash particle size distribution, as well as the cloud top pressure of any underlying water cloud, using an optimal estimation technique applied to Infrared Atmospheric Sounding Interferometer data. Two shapes of particle size distribution are considered, a log-normal and a gamma distribution. Results show that it is viable to retrieve a measure of the size distribution spread, namely the geometric standard deviation, when a log-normal distribution is assumed, whereas this is not the case for an assumed gamma distribution in terms of its effective variance. The volcanic conditions under which the method works well are discussed, as are its shortcomings. The method is applied to two volcanic eruptions: Eyjafjallajökull, Iceland using data from 6th May 2010 and Kasatochi, Alaska using data from 8th August 2008. The results show that the retrieved geometric standard deviation of these ash clouds is spatially variable, and is generally similar to what is assumed in many passive infrared remote sensing techniques. An abrupt change in the retrieved geometric standard deviation has been observed for the Eyjafjallajökull eruption along the trajectory of the ash cloud, and possible explanations for this are discussed. Text Iceland Alaska Copernicus Publications: E-Journals
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description This study demonstrates a method of retrieving the mass column loading and cloud-top pressure of a volcanic ash cloud, together with the effective radius and spread of the ash particle size distribution, as well as the cloud top pressure of any underlying water cloud, using an optimal estimation technique applied to Infrared Atmospheric Sounding Interferometer data. Two shapes of particle size distribution are considered, a log-normal and a gamma distribution. Results show that it is viable to retrieve a measure of the size distribution spread, namely the geometric standard deviation, when a log-normal distribution is assumed, whereas this is not the case for an assumed gamma distribution in terms of its effective variance. The volcanic conditions under which the method works well are discussed, as are its shortcomings. The method is applied to two volcanic eruptions: Eyjafjallajökull, Iceland using data from 6th May 2010 and Kasatochi, Alaska using data from 8th August 2008. The results show that the retrieved geometric standard deviation of these ash clouds is spatially variable, and is generally similar to what is assumed in many passive infrared remote sensing techniques. An abrupt change in the retrieved geometric standard deviation has been observed for the Eyjafjallajökull eruption along the trajectory of the ash cloud, and possible explanations for this are discussed.
format Text
author Western, Luke M.
Francis, Peter N.
Watson, I. Matthew
Mackie, Shona
spellingShingle Western, Luke M.
Francis, Peter N.
Watson, I. Matthew
Mackie, Shona
Inferring the size distribution of volcanic ash from IASI measurements and optimal estimation
author_facet Western, Luke M.
Francis, Peter N.
Watson, I. Matthew
Mackie, Shona
author_sort Western, Luke M.
title Inferring the size distribution of volcanic ash from IASI measurements and optimal estimation
title_short Inferring the size distribution of volcanic ash from IASI measurements and optimal estimation
title_full Inferring the size distribution of volcanic ash from IASI measurements and optimal estimation
title_fullStr Inferring the size distribution of volcanic ash from IASI measurements and optimal estimation
title_full_unstemmed Inferring the size distribution of volcanic ash from IASI measurements and optimal estimation
title_sort inferring the size distribution of volcanic ash from iasi measurements and optimal estimation
publishDate 2018
url https://doi.org/10.5194/amt-2016-92
https://amt.copernicus.org/preprints/amt-2016-92/
genre Iceland
Alaska
genre_facet Iceland
Alaska
op_source eISSN: 1867-8548
op_relation doi:10.5194/amt-2016-92
https://amt.copernicus.org/preprints/amt-2016-92/
op_doi https://doi.org/10.5194/amt-2016-92
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