A Near-Real-Time Method for Estimating Volcanic Ash Emissions Using Satellite Retrievals

We present a Bayesian inversion method for estimating volcanic ash emissions using satellite retrievals of ash column load and an atmospheric dispersion model. An a priori description of the emissions is used based on observations of the rise height of the volcanic plume and a stochastic model of th...

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Published in:Atmosphere
Main Authors: Rachel Pelley, David Thomson, Helen Webster, Michael Cooke, Alistair Manning, Claire Witham, Matthew Hort
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/atmos12121573
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author Rachel Pelley
David Thomson
Helen Webster
Michael Cooke
Alistair Manning
Claire Witham
Matthew Hort
author_facet Rachel Pelley
David Thomson
Helen Webster
Michael Cooke
Alistair Manning
Claire Witham
Matthew Hort
author_sort Rachel Pelley
collection MDPI Open Access Publishing
container_issue 12
container_start_page 1573
container_title Atmosphere
container_volume 12
description We present a Bayesian inversion method for estimating volcanic ash emissions using satellite retrievals of ash column load and an atmospheric dispersion model. An a priori description of the emissions is used based on observations of the rise height of the volcanic plume and a stochastic model of the possible emissions. Satellite data are processed to give column loads where ash is detected and to give information on where we have high confidence that there is negligible ash. An atmospheric dispersion model is used to relate emissions and column loads. Gaussian distributions are assumed for the a priori emissions and for the errors in the satellite retrievals. The optimal emissions estimate is obtained by finding the peak of the a posteriori probability density under the constraint that the emissions are non-negative. We apply this inversion method within a framework designed for use during an eruption with the emission estimates (for any given emission time) being revised over time as more information becomes available. We demonstrate the approach for the 2010 Eyjafjallajökull and 2011 Grímsvötn eruptions. We apply the approach in two ways, using only the ash retrievals and using both the ash and clear sky retrievals. For Eyjafjallajökull we have compared with an independent dataset not used in the inversion and have found that the inversion-derived emissions lead to improved predictions.
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op_doi https://doi.org/10.3390/atmos12121573
op_relation Atmospheric Techniques, Instruments, and Modeling
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op_rights https://creativecommons.org/licenses/by/4.0/
op_source Atmosphere; Volume 12; Issue 12; Pages: 1573
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spelling ftmdpi:oai:mdpi.com:/2073-4433/12/12/1573/ 2025-01-16T21:47:47+00:00 A Near-Real-Time Method for Estimating Volcanic Ash Emissions Using Satellite Retrievals Rachel Pelley David Thomson Helen Webster Michael Cooke Alistair Manning Claire Witham Matthew Hort agris 2021-11-27 application/pdf https://doi.org/10.3390/atmos12121573 EN eng Multidisciplinary Digital Publishing Institute Atmospheric Techniques, Instruments, and Modeling https://dx.doi.org/10.3390/atmos12121573 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 12; Issue 12; Pages: 1573 volcanic ash emissions source inversion atmospheric dispersion satellite ash retrievals Text 2021 ftmdpi https://doi.org/10.3390/atmos12121573 2023-08-01T03:23:27Z We present a Bayesian inversion method for estimating volcanic ash emissions using satellite retrievals of ash column load and an atmospheric dispersion model. An a priori description of the emissions is used based on observations of the rise height of the volcanic plume and a stochastic model of the possible emissions. Satellite data are processed to give column loads where ash is detected and to give information on where we have high confidence that there is negligible ash. An atmospheric dispersion model is used to relate emissions and column loads. Gaussian distributions are assumed for the a priori emissions and for the errors in the satellite retrievals. The optimal emissions estimate is obtained by finding the peak of the a posteriori probability density under the constraint that the emissions are non-negative. We apply this inversion method within a framework designed for use during an eruption with the emission estimates (for any given emission time) being revised over time as more information becomes available. We demonstrate the approach for the 2010 Eyjafjallajökull and 2011 Grímsvötn eruptions. We apply the approach in two ways, using only the ash retrievals and using both the ash and clear sky retrievals. For Eyjafjallajökull we have compared with an independent dataset not used in the inversion and have found that the inversion-derived emissions lead to improved predictions. Text Eyjafjallajökull MDPI Open Access Publishing Atmosphere 12 12 1573
spellingShingle volcanic ash emissions
source inversion
atmospheric dispersion
satellite ash retrievals
Rachel Pelley
David Thomson
Helen Webster
Michael Cooke
Alistair Manning
Claire Witham
Matthew Hort
A Near-Real-Time Method for Estimating Volcanic Ash Emissions Using Satellite Retrievals
title A Near-Real-Time Method for Estimating Volcanic Ash Emissions Using Satellite Retrievals
title_full A Near-Real-Time Method for Estimating Volcanic Ash Emissions Using Satellite Retrievals
title_fullStr A Near-Real-Time Method for Estimating Volcanic Ash Emissions Using Satellite Retrievals
title_full_unstemmed A Near-Real-Time Method for Estimating Volcanic Ash Emissions Using Satellite Retrievals
title_short A Near-Real-Time Method for Estimating Volcanic Ash Emissions Using Satellite Retrievals
title_sort near-real-time method for estimating volcanic ash emissions using satellite retrievals
topic volcanic ash emissions
source inversion
atmospheric dispersion
satellite ash retrievals
topic_facet volcanic ash emissions
source inversion
atmospheric dispersion
satellite ash retrievals
url https://doi.org/10.3390/atmos12121573