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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Bibliographic Details
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
Description
Summary:<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>
ISSN:1593-5213
2037-416X