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<front>
<journal-meta>
<journal-id journal-id-type="publisher">AMT</journal-id>
<journal-title-group>
<journal-title>Atmospheric Measurement Techniques</journal-title>
<abbrev-journal-title abbrev-type="publisher">AMT</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Meas. Tech.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1867-8548</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/amt-6-3539-2013</article-id>
<title-group>
<article-title>SAGE version 7.0 algorithm: application to SAGE II</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Damadeo</surname>
<given-names>R. P.</given-names>
<ext-link>https://orcid.org/0000-0002-1466-839X</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zawodny</surname>
<given-names>J. M.</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>Thomason</surname>
<given-names>L. W.</given-names>
<ext-link>https://orcid.org/0000-0002-1902-0840</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Iyer</surname>
<given-names>N.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>NASA Langley Research Center, Hampton, VA, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Science Systems and Applications Inc., Hampton, VA, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>17</day>
<month>12</month>
<year>2013</year>
</pub-date>
<volume>6</volume>
<issue>12</issue>
<fpage>3539</fpage>
<lpage>3561</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 R. P. Damadeo et al.</copyright-statement>
<copyright-year>2013</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://amt.copernicus.org/articles/6/3539/2013/amt-6-3539-2013.html">This article is available from https://amt.copernicus.org/articles/6/3539/2013/amt-6-3539-2013.html</self-uri>
<self-uri xlink:href="https://amt.copernicus.org/articles/6/3539/2013/amt-6-3539-2013.pdf">The full text article is available as a PDF file from https://amt.copernicus.org/articles/6/3539/2013/amt-6-3539-2013.pdf</self-uri>
<abstract>
<p>This paper details the SAGE (Stratospheric Aerosol and Gas Experiment) version 7.0 algorithm and how it is applied to
SAGE II. Changes made between the previous (v6.2) and current (v7.0) versions
are described and their impacts on the data products explained for both
coincident event comparisons and time-series analysis. Users of the data will
notice a general improvement in all of the SAGE II data products, which are
now in better agreement with more modern data sets (e.g., SAGE III) and more
robust for use with trend studies.</p>
</abstract>
<counts><page-count count="23"/></counts>
</article-meta>
</front>
<body/>
<back>
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