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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-9-6827-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/6827/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/6827/2009/acpd-9-6827-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/6827/2009/acpd-9-6827-2009.pdf</fulltext_pdf>
	<start_page>6827</start_page>
	<end_page>6854</end_page>
	<publication_date>2009-03-11</publication_date>
	<article_title content_type="html">Vertical distribution of aerosols in Mexico City during MILAGRO-2006 campaign</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>P. A. Lewandowski</name>
			<email>piotr-lewandowski@uiowa.edu</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>W. E. Eichinger</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>H. Holder</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>J. Prueger</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">IIHR-Hydroscience &amp; Engineering, University of Iowa, Iowa City, Iowa 52242, USA</affiliation>
		<affiliation numeration="2" content_type="html">Duke University, Rayleigh, NC, USA</affiliation>
		<affiliation numeration="3" content_type="html">National Soil Tilth Laboratory, Ames, IA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">On 7 March 2006, a mobile, ground-based, vertical pointing, elastic
  lidar system made a North-South transect through the Mexico City
  basin.  Aerosol size distribution measurements, made concurrently,
  allowed calculation of the mass extinction efficiency (MEE)
  for the lidar system (1064 nm). MEE combined with
  an inverted lidar extinction coefficient resulted in total aerosol
  vertical mass estimates with 1.5 m vertical spatial and
  1 s temporal resolution.
&lt;br&gt;&lt;br&gt;
  The results showed that the aerosol loading within the basin is
  about twice what is observed outside of the basin. The total aerosol
  base concentrations observed in the basin are of the order of
  200 &amp;mu;g/m&lt;sup&gt;3&lt;/sup&gt; and the base levels outside are of the order
  of 100 &amp;mu;g/m&lt;sup&gt;3&lt;/sup&gt;. The local heavy traffic events can
  introduce aerosol levels near the ground as high as 900 &amp;mu;g/m&lt;sup&gt;3&lt;/sup&gt;. The lidar-based total aerosol loading compares with the
  hourly-averaged PM&lt;sub&gt;10&lt;/sub&gt; ground observations conducted by the RAMA
  monitoring network throughout Mexico City.</abstract>
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</article>

