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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>8</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-3761-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/3761/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/3761/2008/acpd-8-3761-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/3761/2008/acpd-8-3761-2008.pdf</fulltext_pdf>
	<start_page>3761</start_page>
	<end_page>3805</end_page>
	<publication_date>2008-02-25</publication_date>
	<article_title content_type="html">Estimation of the vertical profile of sulfur dioxide injection into the  atmosphere by a volcanic eruption using satellite column measurements and inverse transport modeling</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>S. Eckhardt</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>A. J. Prata</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>P. Seibert</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>K. Stebel</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>A. Stohl</name>
			<email>ast@nilu.no</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Norwegian Institute for Air Research, Kjeller, Norway</affiliation>
		<affiliation numeration="2" content_type="html">Inst. of Meteorology, Univ. of Natural Resources and Applied Life Sciences, Vienna, Austria</affiliation>
	</affiliations>
	<abstract content_type="html">An analytical inversion method has been developed to estimate the vertical profile of SO&lt;sub&gt;2&lt;/sub&gt; emissions from volcanic eruptions.
The method uses satellite-observed total SO&lt;sub&gt;2&lt;/sub&gt; columns and an atmospheric transport model (FLEXPART)
to exploit the fact that winds change with altitude &amp;ndash; thus, the position and
shape of the volcanic plume bear information on its emission altitude.
The method finds the vertical emission distribution which minimizes the total
difference between simulated and observed  SO&lt;sub&gt;2&lt;/sub&gt; columns while also considering a priori information.
We have tested the method with the eruption of Jebel at Tair on 30 September 2007
for which a comprehensive observational data set from various satellite instruments
(AIRS, OMI, SEVIRI, CALIPSO) is available.
Using satellite data from the first 24 h after the eruption for the inversion,
we found an emission maximum near 16 km above sea level (asl), and secondary maxima near 5, 9, 12 and 14 km a.s.l.
60% of the emission occurred above the tropopause.
The emission profile obtained in the inversion was then used to simulate the transport
of the plume over the following week.
The modeled plume agrees very well with SO&lt;sub&gt;2&lt;/sub&gt; total columns observed by OMI, and its
altitude and width agree mostly within 1&amp;ndash;2 km with CALIPSO observations of stratospheric
aerosol produced from the SO&lt;sub&gt;2&lt;/sub&gt;.
The inversion result is robust against various changes in both the a priori and the
observations.
Even when using only SEVIRI data from the first 15 h after the eruption, the emission
profile was reasonably well estimated.
The method is computationally very fast.
It is therefore suitable for implementation within an operational environment, such as the
Volcanic Ash Advisory Centers, to predict the threat posed by volcanic ash for air traffic.
It could also be helpful for assessing the sulfur input into the stratosphere, be it in the
context of volcanic processes or also for proposed geo-engineering techniques to counteract global warming.</abstract>
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</article>

