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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-9-8817-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/8817/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/8817/2009/acpd-9-8817-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/8817/2009/acpd-9-8817-2009.pdf</fulltext_pdf>
	<start_page>8817</start_page>
	<end_page>8856</end_page>
	<publication_date>2009-04-02</publication_date>
	<article_title content_type="html">NASA LaRC airborne high spectral resolution lidar aerosol measurements during  MILAGRO: observations and validation</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>R. R. Rogers</name>
			<email>raymond.r.rogers@nasa.gov</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. W. Hair</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>C. A. Hostetler</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>R. A. Ferrare</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>M. D. Obland</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>A. L. Cook</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>D. B. Harper</name>
		</author>
		<author numeration="8" affiliations="2">
			<name>S. P. Burton</name>
		</author>
		<author numeration="9" affiliations="3,5">
			<name>Y. Shinozuka</name>
		</author>
		<author numeration="10" affiliations="3">
			<name>C. S. McNaughton</name>
		</author>
		<author numeration="11" affiliations="3">
			<name>A. D. Clarke</name>
		</author>
		<author numeration="12" affiliations="4">
			<name>J. Redemann</name>
		</author>
		<author numeration="13" affiliations="5">
			<name>P. B. Russell</name>
		</author>
		<author numeration="14" affiliations="6">
			<name>J. M. Livingston</name>
		</author>
		<author numeration="15" affiliations="7">
			<name>L. I. Kleinman</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">NASA Langley Research Center, Hampton, VA, USA</affiliation>
		<affiliation numeration="2" content_type="html">SSAI/NASA Langley Research Center, Hampton, VA, USA</affiliation>
		<affiliation numeration="3" content_type="html">University of Hawaii, Dept. of Oceanography, Honolulu, HI, USA</affiliation>
		<affiliation numeration="4" content_type="html">BAERI/NASA Ames Research Center, Moffett Field, CA, USA</affiliation>
		<affiliation numeration="5" content_type="html">NASA Ames Research Center, Moffett Field, CA, USA</affiliation>
		<affiliation numeration="6" content_type="html">SRI International/NASA Ames Research Center, Moffett Field, CA, USA</affiliation>
		<affiliation numeration="7" content_type="html">Brookhaven National Laboratory, USA</affiliation>
	</affiliations>
	<abstract content_type="html">The NASA Langley Research Center (LaRC) airborne High Spectral
      Resolution Lidar (HSRL) measures vertical profiles of aerosol
      extinction, backscatter, and depolarization at both 532 nm and
      1064 nm. In March of 2006 the HSRL participated in the
      Megacity Initiative: Local and Global Research Observations (MILAGRO)
      campaign along with several other suites of instruments deployed on
      both aircraft and ground based platforms. This paper presents high
      spatial and vertical resolution HSRL measurements of aerosol
      extinction and optical depth from MILAGRO and comparisons of those
      measurements with similar measurements from other sensors and model
      predictions. HSRL measurements coincident with airborne in situ
      aerosol scattering and absorption measurements from two different
      instrument suites on the C-130 and G-1 aircraft, airborne aerosol
      optical depth (AOD) and extinction measurements from an airborne
      tracking sunphotometer on the J-31 aircraft, and AOD from a network of
      ground based Aerosol Robotic Network (AERONET) sun photometers are
      presented as a validation of the HSRL aerosol extinction and optical
      depth products. Regarding the extinction validation, we find bias
      differences between HSRL and these instruments to be less than 3%
      (0.01 km&lt;sup&gt;&amp;minus;1&lt;/sup&gt;) at 532 nm, the wavelength at which the
      HSRL technique is employed. The rms differences at 532 nm were
      less than 50% (0.015 km&lt;sup&gt;&amp;minus;1&lt;/sup&gt;). To our knowledge this is the
      most comprehensive validation of the HSRL measurement of aerosol
      extinction and optical depth to date. The observed bias differences in
      ambient aerosol extinction between HSRL and other measurements is
      within 15–20% at visible wavelengths, found by previous studies to
      be the differences observed with current state-of-the-art
      instrumentation (Schmid et al., 2006).</abstract>
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</article>

