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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>2</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-4831-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/4831/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/4831/2008/acpd-8-4831-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/4831/2008/acpd-8-4831-2008.pdf</fulltext_pdf>
	<start_page>4831</start_page>
	<end_page>4876</end_page>
	<publication_date>2008-03-05</publication_date>
	<article_title content_type="html">Characterization of the South Atlantic marine boundary layer aerosol using an Aerodyne Aerosol Mass Spectrometer</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>S. R. Zorn</name>
			<email>zorns@mpch-mainz.mpg.de</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>F. Drewnick</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>M. Schott</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>T. Hoffmann</name>
		</author>
		<author numeration="5" affiliations="1,2">
			<name>S. Borrmann</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Max Planck Institute for Chemistry, Particle Chemistry Department, Mainz, Germany</affiliation>
		<affiliation numeration="2" content_type="html">University of Mainz, Institute for Atmospheric Physics, Mainz, Germany</affiliation>
		<affiliation numeration="3" content_type="html">University of Mainz, Institute of Inorganic and Analytical Chemistry, Mainz, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">Measurements of the submicron fraction of the atmospheric aerosol in the
marine boundary layer were performed from January to March 2007 (Southern
Hemisphere summer) onboard the French research vessel Marion Dufresne in the
Southern Atlantic and Indian Ocean (20&amp;deg; S&amp;ndash;60&amp;deg; S,
70&amp;deg; W&amp;ndash;60&amp;deg; E). For chemical composition measurements an Aerodyne
High-Resolution-Time-of-Flight AMS was used to measure mass concentrations
and species-resolved size distributions of non-refractory aerosol components
in the submicron range.

&lt;br&gt;&lt;br&gt;

 Within the &quot;standard&quot; AMS compounds (ammonium,
chloride, nitrate, sulfate, organics) &quot;sulfate&quot; is the dominating species in
the marine boundary layer reaching concentrations between 50 ng m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; and
3 μg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;. Furthermore, what is seen as &quot;sulfate&quot; by the AMS seems
to be mostly sulfuric acid. Another sulfur containing species that can
ubiquitously be found in marine environments is methanesulfonic acid (MSA).
Since MSA has not been directly measured before with an AMS, and is not part
of the standard AMS analysis, laboratory experiments needed to be performed
in order to be able to identify it within the AMS raw data and to extract
mass concentrations for MSA from the field measurements. To identify
characteristic air masses and their source regions backwards trajectories
were used and averaged concentrations for AMS standard compounds were
calculated for each air mass type. Sulfate mass size distributions were
measured for these periods showing a distinct difference between oceanic air
masses and those from African outflow. While the peak size in the mass
distribution was roughly 250 nm in marine air masses it was shifted to 470 nm in African outflow
air. Correlations between the mass concentrations of sulfate, organics and
MSA were calculated which show a narrow correlation for MSA with
sulfate/sulfuric acid coming from the ocean but not with continental sulfate.</abstract>
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</article>

