WRF-Chem modeling of sulfur dioxide emissions from the 2008 Kasatochi Volcano

<div class="page" title="Page 1"><div class="section"><div class="layoutArea"><div class="column"><p><span>We simulate the dispersion and chemical evolution of the sulfur dioxide (SO</span><span>2</s...

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Main Authors: Sean David Egan, Martin Stuefer, Peter Webley, Catherine F. Cahill
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2015-03-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/6626
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spelling doaj-b919253c5c5242b1aba57e1b42a24cf02020-11-25T00:35:47ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2015-03-0157010.4401/ag-66265981WRF-Chem modeling of sulfur dioxide emissions from the 2008 Kasatochi VolcanoSean David Egan0Martin Stuefer1Peter Webley2Catherine F. Cahill3University of Alaska Fairbanks, Geophysical Institute and College of Natural Sciences and Mathematics, FairbanksUniversity of Alaska Fairbanks, Geophysical Institute, Fairbanks,University of Alaska Fairbanks, Geophysical Institute, FairbanksUniversity of Alaska Fairbanks, Geophysical Institute and College of Natural Sciences and Mathematics, Fairbanks<div class="page" title="Page 1"><div class="section"><div class="layoutArea"><div class="column"><p><span>We simulate the dispersion and chemical evolution of the sulfur dioxide (SO</span><span>2</span><span>) plume following the eruption of Kasatochi Volcano in Alaska, USA, on August 7</span><span>th</span><span>, 2008 with the Weather Research Forecasting with Chemistry (WRF-Chem) model. The model was initialized with the observed three distinct plumes, which were characterized by a total estimated SO</span><span>2 </span><span>mass of 0.5 to 2.7 Tg. WRF-Chem modeled output was compared to remote sensing retrievals from the Ozone Monitoring Instrument (OMI), and the modeled plumes agreed well in shape and location with the OMI retrievals. The calculated SO</span><span>2 </span><span>column densities showed comparable Dobson Unit values with higher densities especially in the center of the distal plume over northern Canada. We concluded from our analysis that WRF-Chem derived a 9.1-day lifetime of the SO</span><span>2 </span><span>when initialized with a 12km eruption height. Sensitivity tests with varying eruption plume heights revealed significantly in- creased lifetimes of SO</span><span>2 </span><span>up to 17.1 days for higher plumes. </span></p></div></div></div></div>http://www.annalsofgeophysics.eu/index.php/annals/article/view/6626WRF-Chem, volcano, sulfur dioxide, model, emissions
collection DOAJ
language English
format Article
sources DOAJ
author Sean David Egan
Martin Stuefer
Peter Webley
Catherine F. Cahill
spellingShingle Sean David Egan
Martin Stuefer
Peter Webley
Catherine F. Cahill
WRF-Chem modeling of sulfur dioxide emissions from the 2008 Kasatochi Volcano
Annals of Geophysics
WRF-Chem, volcano, sulfur dioxide, model, emissions
author_facet Sean David Egan
Martin Stuefer
Peter Webley
Catherine F. Cahill
author_sort Sean David Egan
title WRF-Chem modeling of sulfur dioxide emissions from the 2008 Kasatochi Volcano
title_short WRF-Chem modeling of sulfur dioxide emissions from the 2008 Kasatochi Volcano
title_full WRF-Chem modeling of sulfur dioxide emissions from the 2008 Kasatochi Volcano
title_fullStr WRF-Chem modeling of sulfur dioxide emissions from the 2008 Kasatochi Volcano
title_full_unstemmed WRF-Chem modeling of sulfur dioxide emissions from the 2008 Kasatochi Volcano
title_sort wrf-chem modeling of sulfur dioxide emissions from the 2008 kasatochi volcano
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 2015-03-01
description <div class="page" title="Page 1"><div class="section"><div class="layoutArea"><div class="column"><p><span>We simulate the dispersion and chemical evolution of the sulfur dioxide (SO</span><span>2</span><span>) plume following the eruption of Kasatochi Volcano in Alaska, USA, on August 7</span><span>th</span><span>, 2008 with the Weather Research Forecasting with Chemistry (WRF-Chem) model. The model was initialized with the observed three distinct plumes, which were characterized by a total estimated SO</span><span>2 </span><span>mass of 0.5 to 2.7 Tg. WRF-Chem modeled output was compared to remote sensing retrievals from the Ozone Monitoring Instrument (OMI), and the modeled plumes agreed well in shape and location with the OMI retrievals. The calculated SO</span><span>2 </span><span>column densities showed comparable Dobson Unit values with higher densities especially in the center of the distal plume over northern Canada. We concluded from our analysis that WRF-Chem derived a 9.1-day lifetime of the SO</span><span>2 </span><span>when initialized with a 12km eruption height. Sensitivity tests with varying eruption plume heights revealed significantly in- creased lifetimes of SO</span><span>2 </span><span>up to 17.1 days for higher plumes. </span></p></div></div></div></div>
topic WRF-Chem, volcano, sulfur dioxide, model, emissions
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/6626
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