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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-11-3673-2011</article-id>
<title-group>
<article-title>Airborne observation of aerosol optical depth during ARCTAS:  vertical profiles, inter-comparison and fine-mode fraction</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Shinozuka</surname>
<given-names>Y.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Redemann</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Livingston</surname>
<given-names>J. M.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Russell</surname>
<given-names>P. B.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Clarke</surname>
<given-names>A. D.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Howell</surname>
<given-names>S. G.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Freitag</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>O&apos;Neill</surname>
<given-names>N. T.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Reid</surname>
<given-names>E. A.</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Johnson</surname>
<given-names>R.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ramachandran</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>McNaughton</surname>
<given-names>C. S.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
<xref ref-type="aff" rid="aff11">
<sup>11</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kapustin</surname>
<given-names>V. N.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Brekhovskikh</surname>
<given-names>V.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Holben</surname>
<given-names>B. N.</given-names>
</name>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>McArthur</surname>
<given-names>L. J. B.</given-names>
</name>
<xref ref-type="aff" rid="aff10">
<sup>10</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>NASA Postdoctoral Program, NASA Ames Research Center, Moffett Field, California, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Bay Area Environmental Research Institute, Sonoma, California, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>SRI International, Menlo Park, California, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>NASA Ames Research Center, Moffett Field, California, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>School of Ocean and Earth Science and Technology, University of Hawaii, Honolulu, Hawaii, USA</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>CARTEL, Université de Sherbrooke, Sherbrooke, Québec, Canada</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>Marine Meteorology Division, Naval Research Laboratory, Monterey, California, USA</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>Physical Research Laboratory, Ahmedabad, India</addr-line>
</aff>
<aff id="aff9">
<label>9</label>
<addr-line>NASA Goddard Space Flight Center, Greenbelt, Maryland, USA</addr-line>
</aff>
<aff id="aff10">
<label>10</label>
<addr-line>Environment Canada, Toronto, Ontario, Canada</addr-line>
</aff>
<aff id="aff11">
<label>11</label>
<addr-line>now at: Aina Kai Environmental, LLC, Aiea, Hawaii, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>20</day>
<month>04</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>8</issue>
<fpage>3673</fpage>
<lpage>3688</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/3673/2011/acp-11-3673-2011.html">This article is available from http://www.atmos-chem-phys.net/11/3673/2011/acp-11-3673-2011.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/3673/2011/acp-11-3673-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/3673/2011/acp-11-3673-2011.pdf</self-uri>
<abstract>
<p>We describe aerosol optical depth (AOD) measured during the Arctic Research
of the Composition of the Troposphere from Aircraft and Satellites (ARCTAS)
experiment, focusing on vertical profiles, inter-comparison with correlative
observations and fine-mode fraction. Arctic haze observed in &lt;2 km and 2–4 km over Alaska in April 2008 originated mainly from anthropogenic emission
and biomass burning, respectively, according to aerosol mass spectrometry
and black carbon incandescence measurements. The Ångström exponent for these
air masses is 1.4 ± 0.3 and 1.7 ± 0.1, respectively, when derived at
499 nm from a second-order polynomial fit to the AOD spectra measured with
the 14-channel Ames Airborne Tracking Sunphotometer (AATS-14) over 354–2139 nm. We examine 55 vertical profiles selected from all phases of the
experiment. For two thirds of them, the AOD spectra are within 3% + 0.02 of
the vertical integral of local visible-light scattering and absorption. The
horizontal structure of smoke plumes from local biomass burning observed in
central Canada in June and July 2008 explains most outliers. The differences
in mid-visible Ångström exponent are &lt;0.10 for 63% of the profiles with
499-nm AOD &gt; 0.1. The retrieved fine-mode fraction of AOD is mostly between
0.7 and 1.0, and its root mean square difference (in both directions) from
column-integral submicron fraction (measured with nephelometers, absorption
photometers and an impactor) is 0.12. These AOD measurements from the NASA
P-3 aircraft, after compensation for below-aircraft light attenuation by
vertical extrapolation, mostly fall within ±0.02 of AERONET
ground-based measurements between 340–1640 nm for five overpass events.</p>
</abstract>
<counts><page-count count="16"/></counts>
</article-meta>
</front>
<body/>
<back>
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