Operational Modelling of Umbrella Cloud Growth in a Lagrangian Volcanic Ash Transport and Dispersion Model

Large explosive eruptions can result in the formation of an umbrella cloud which rapidly expands, spreading ash out radially from the volcano. The lateral spread by the intrusive gravity current dominates the transport of the ash cloud. Hence, to accurately forecast the transport of ash from large e...

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Published in:Atmosphere
Main Authors: Helen N. Webster, Benjamin J. Devenish, Larry G. Mastin, David J. Thomson, Alexa R. Van Eaton
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2020
Subjects:
Online Access:https://doi.org/10.3390/atmos11020200
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spelling ftmdpi:oai:mdpi.com:/2073-4433/11/2/200/ 2023-08-20T04:06:21+02:00 Operational Modelling of Umbrella Cloud Growth in a Lagrangian Volcanic Ash Transport and Dispersion Model Helen N. Webster Benjamin J. Devenish Larry G. Mastin David J. Thomson Alexa R. Van Eaton agris 2020-02-13 application/pdf https://doi.org/10.3390/atmos11020200 EN eng Multidisciplinary Digital Publishing Institute Air Quality https://dx.doi.org/10.3390/atmos11020200 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 11; Issue 2; Pages: 200 umbrella cloud volcanic ash transport and dispersion model lateral spread satellite observations operational forecasting Text 2020 ftmdpi https://doi.org/10.3390/atmos11020200 2023-07-31T23:06:47Z Large explosive eruptions can result in the formation of an umbrella cloud which rapidly expands, spreading ash out radially from the volcano. The lateral spread by the intrusive gravity current dominates the transport of the ash cloud. Hence, to accurately forecast the transport of ash from large eruptions, lateral spread of umbrella clouds needs to be represented within volcanic ash transport and dispersion models. Here, we describe an umbrella cloud parameterisation which has been implemented into an operational Lagrangian model and consider how it may be used during an eruption when information concerning the eruption is limited and model runtime is key. We examine different relations for the volume flow rate into the umbrella, and the rate of spreading within the cloud. The scheme is validated against historic eruptions of differing scales (Pinatubo 1991, Kelud 2014, Calbuco 2015 and Eyjafjallajökull 2010) by comparing model predictions with satellite observations. Reasonable predictions of umbrella cloud spread are achieved using an estimated volume flow rate from the empirical equation by Bursik et al. and the observed eruption height. We show how model predictions can be refined during an ongoing eruption as further information and observations become available. Text Eyjafjallajökull MDPI Open Access Publishing Bursik ENVELOPE(-84.383,-84.383,-79.717,-79.717) Atmosphere 11 2 200
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic umbrella cloud
volcanic ash transport and dispersion model
lateral spread
satellite observations
operational forecasting
spellingShingle umbrella cloud
volcanic ash transport and dispersion model
lateral spread
satellite observations
operational forecasting
Helen N. Webster
Benjamin J. Devenish
Larry G. Mastin
David J. Thomson
Alexa R. Van Eaton
Operational Modelling of Umbrella Cloud Growth in a Lagrangian Volcanic Ash Transport and Dispersion Model
topic_facet umbrella cloud
volcanic ash transport and dispersion model
lateral spread
satellite observations
operational forecasting
description Large explosive eruptions can result in the formation of an umbrella cloud which rapidly expands, spreading ash out radially from the volcano. The lateral spread by the intrusive gravity current dominates the transport of the ash cloud. Hence, to accurately forecast the transport of ash from large eruptions, lateral spread of umbrella clouds needs to be represented within volcanic ash transport and dispersion models. Here, we describe an umbrella cloud parameterisation which has been implemented into an operational Lagrangian model and consider how it may be used during an eruption when information concerning the eruption is limited and model runtime is key. We examine different relations for the volume flow rate into the umbrella, and the rate of spreading within the cloud. The scheme is validated against historic eruptions of differing scales (Pinatubo 1991, Kelud 2014, Calbuco 2015 and Eyjafjallajökull 2010) by comparing model predictions with satellite observations. Reasonable predictions of umbrella cloud spread are achieved using an estimated volume flow rate from the empirical equation by Bursik et al. and the observed eruption height. We show how model predictions can be refined during an ongoing eruption as further information and observations become available.
format Text
author Helen N. Webster
Benjamin J. Devenish
Larry G. Mastin
David J. Thomson
Alexa R. Van Eaton
author_facet Helen N. Webster
Benjamin J. Devenish
Larry G. Mastin
David J. Thomson
Alexa R. Van Eaton
author_sort Helen N. Webster
title Operational Modelling of Umbrella Cloud Growth in a Lagrangian Volcanic Ash Transport and Dispersion Model
title_short Operational Modelling of Umbrella Cloud Growth in a Lagrangian Volcanic Ash Transport and Dispersion Model
title_full Operational Modelling of Umbrella Cloud Growth in a Lagrangian Volcanic Ash Transport and Dispersion Model
title_fullStr Operational Modelling of Umbrella Cloud Growth in a Lagrangian Volcanic Ash Transport and Dispersion Model
title_full_unstemmed Operational Modelling of Umbrella Cloud Growth in a Lagrangian Volcanic Ash Transport and Dispersion Model
title_sort operational modelling of umbrella cloud growth in a lagrangian volcanic ash transport and dispersion model
publisher Multidisciplinary Digital Publishing Institute
publishDate 2020
url https://doi.org/10.3390/atmos11020200
op_coverage agris
long_lat ENVELOPE(-84.383,-84.383,-79.717,-79.717)
geographic Bursik
geographic_facet Bursik
genre Eyjafjallajökull
genre_facet Eyjafjallajökull
op_source Atmosphere; Volume 11; Issue 2; Pages: 200
op_relation Air Quality
https://dx.doi.org/10.3390/atmos11020200
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos11020200
container_title Atmosphere
container_volume 11
container_issue 2
container_start_page 200
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