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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-7-3341-2007</article-id>
<title-group>
<article-title>Aerosol single-scattering albedo and asymmetry parameter from MFRSR observations during the ARM Aerosol IOP 2003</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kassianov</surname>
<given-names>E. I.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Flynn</surname>
<given-names>C. J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ackerman</surname>
<given-names>T. P.</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>Barnard</surname>
<given-names>J. C.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Pacific Northwest National Laboratory, Richland, 99352, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>University of Washington, Seattle, 98195, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>27</day>
<month>06</month>
<year>2007</year>
</pub-date>
<volume>7</volume>
<issue>12</issue>
<fpage>3341</fpage>
<lpage>3351</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/7/3341/2007/acp-7-3341-2007.html">This article is available from http://www.atmos-chem-phys.net/7/3341/2007/acp-7-3341-2007.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/7/3341/2007/acp-7-3341-2007.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/7/3341/2007/acp-7-3341-2007.pdf</self-uri>
<abstract>
<p>Multi-filter Rotating Shadowband Radiometers (MFRSRs) provide routine
measurements of the aerosol optical depth (τ) at six wavelengths
(0.415, 0.5, 0.615, 0.673, 0.870 and 0.94 μm). The single-scattering
albedo (&amp;pi;&lt;sub&gt;0&lt;/sub&gt;) is typically estimated from the MFRSR measurements by
assuming the asymmetry parameter (&lt;I&gt;g&lt;/I&gt;). In most instances, however, it is
not easy to set an appropriate value of &lt;I&gt;g&lt;/I&gt; due to its strong temporal and
spatial variability. Here, we introduce and validate an updated version of
our retrieval technique that allows one to estimate simultaneously &amp;pi;&lt;sub&gt;0&lt;/sub&gt; and 
&lt;I&gt;g&lt;/I&gt; for different types of aerosol. We use the aerosol and
radiative properties obtained during the Atmospheric Radiation Measurement
(ARM) Program&apos;s Aerosol Intensive Operational Period (IOP) to validate our
retrieval in two ways. First, the MFRSR-retrieved optical properties are
compared with those obtained from independent surface, Aerosol Robotic
Network (AERONET), and aircraft measurements. The MFRSR-retrieved optical
properties are in reasonable agreement with these independent measurements.
Second, we perform radiative closure experiments using the MFRSR-retrieved
optical properties. The calculated broadband values of the direct and
diffuse fluxes are comparable (~5 W/m&lt;sup&gt;2&lt;/sup&gt;) to those obtained from
measurements.</p>
</abstract>
<counts><page-count count="11"/></counts>
</article-meta>
</front>
<body/>
<back>
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