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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>9</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-9399-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/9399/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/9399/2009/acpd-9-9399-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/9399/2009/acpd-9-9399-2009.pdf</fulltext_pdf>
	<start_page>9399</start_page>
	<end_page>9456</end_page>
	<publication_date>2009-04-09</publication_date>
	<article_title content_type="html">Aerosol composition of the tropical upper troposphere</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>K. D. Froyd</name>
			<email>karl.froyd@noaa.gov</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>D. M. Murphy</name>
		</author>
		<author numeration="3" affiliations="1,2">
			<name>T. J. Sanford</name>
		</author>
		<author numeration="4" affiliations="1,2">
			<name>D. S. Thomson</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>J. C. Wilson</name>
		</author>
		<author numeration="6" affiliations="4">
			<name>L. Pfister</name>
		</author>
		<author numeration="7" affiliations="5">
			<name>L. Lait</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">NOAA Earth System Research Laboratory, Chemical Sciences Division,  Boulder, CO, USA</affiliation>
		<affiliation numeration="2" content_type="html">Cooperative Inst. for Res. in Environ. Science, University of  Colorado, Boulder, CO, USA</affiliation>
		<affiliation numeration="3" content_type="html">Dept.~of Mechanical and Materials Engineering, University of Denver,  Denver, CO, USA</affiliation>
		<affiliation numeration="4" content_type="html">NASA Ames Research Center, Moffett Field, CA, USA</affiliation>
		<affiliation numeration="5" content_type="html">Goddard Earth Sciences and Technology Center, University of Maryland Baltimore  County, Baltimore, MD, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Aerosol composition was measured by the NOAA single particle mass
      spectrometer (PALMS) aboard the NASA WB-57 high altitude aircraft
      platform during two Aura Validation Experiment (AVE) campaigns based
      in Costa Rica in 2004 and 2006. These studies yielded the most
      complete set of aerosol composition measurements to date throughout
      the tropical tropopause layer (TTL) and tropical lower
      stratosphere. We describe the aerosol properties of the tropical
      atmosphere and use composition tracers to examine particle sources,
      the role of recent convection, and cirrus-forming potential in the
      TTL. Tropical dynamics and regional air sources played principal roles
      in dictating tropospheric aerosol properties. There was a sharp change
      in aerosol chemical composition at about 12 km altitude
      coincident with a change in convective influence. Below this level,
      maritime convection lofted condensable material that generated acidic,
      sulfate-rich aerosol. These particles contained significant amounts of
      methanesulfonic acid (MSA) and showed evidence of cloud processes. In
      contrast, continental convection injected particles and precursors
      directly into the TTL, yielding a population of neutralized,
      organic-rich aerosol. The organics were often highly oxidized and
      particles with oxidized organics also contained nitrate. Above the
      tropopause, chemical composition gradually changed toward sulfuric
      acid particles but neutralized particles were still abundant
      2 km above the tropopause. Deep continental convection, though
      sporadic and geographically localized, may strongly influence TTL
      aerosol properties on a global scale. The abundance of organic-rich
      aerosol may inhibit ice nucleation and formation of tropopause level
      cirrus.</abstract>
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