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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</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/acpd-11-5493-2011</article-id>
<title-group>
<article-title>The influence of semi-volatile and reactive primary emissions on the abundance and properties of global organic aerosol</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Jathar</surname>
<given-names>S. H.</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>Farina</surname>
<given-names>S. C.</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>Robinson</surname>
<given-names>A. L.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Adams</surname>
<given-names>P. J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Engineering and Public Policy, Carnegie Mellon University, Pittsburgh,  PA 15213, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Chemical Engineering, Carnegie Mellon University, Pittsburgh, PA, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Mechanical Engineering, Carnegie Mellon University, Pittsburgh,  PA 15213, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Department of Civil and Environmental Engineering, Carnegie Mellon University, Pittsburgh, PA 15213, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>15</day>
<month>02</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>2</issue>
<fpage>5493</fpage>
<lpage>5540</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>
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<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/11/5493/2011/acpd-11-5493-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/11/5493/2011/acpd-11-5493-2011.pdf</self-uri>
<abstract>
<p>Semi-volatile and reactive primary organic aerosols are modeled on a global
scale using the GISS GCM II&apos; &quot;unified&quot; climate model. We employ the
volatility basis set framework to simulate emissions, chemical reactions and
phase partitioning of primary and secondary
 organic aerosol (POA and SOA). The model also incorporates the emissions and reactions of
  intermediate volatility organic compounds (IVOCs) as a source of OA, one that has been
   missing in most prior work. Model predictions are evaluated against a broad set of
   observational constraints including mass concentrations, degree of oxygenation, volatility
   and isotopic composition. A traditional model that treats POA as non-volatile and non-reactive
   is also compared to the same set of observations to highlight the progress made in this effort.
    The revised model predicts a global dominance of SOA and brings the POA/SOA split into better
     agreement with ambient measurements. This change is due to traditionally defined POA evaporating
     and the evaporated vapors oxidizing to form non-traditional SOA. IVOCs (traditionally not included
     in chemical transport models) oxidize to form condensable products that account for a third of total
      OA, suggesting that global models have been missing a large source of OA. Predictions of the revised model
       for the oxygenated OA (OOA) fraction at 17 different locations and OA volatility at 3 different locations
        compared much better to observations than predictions from the traditional model. When compared against
         monthly averaged OA mass concentrations measured by the IMPROVE network, model predictions lied within
          a factor of two in summer and mostly within a factor of five during winter. A sensitivity analysis
          indicates that the winter comparison can be improved either by increasing POA emissions or lowering
           the volatility of those emissions. Model predictions of the isotopic composition
           of OA are compared against those computed via a radiocarbon isotope analysis of
           field samples. The contemporary fraction, on average, is slightly under-predicted (20%)
           during the summer months but is a factor of two lower during the winter months. We hypothesize
           that the large wintertime under-prediction of surface OA mass concentrations and the
           contemporary fraction is due to an under-representation of biofuel (particularly,
           residential wood burning) emissions in the emission inventory. Overall, the model
           evaluation highlights the importance of treating POA as semi-volatile and reactive
           in order to predict accurately the sources, composition and properties of ambient OA.</p>
</abstract>
<counts><page-count count="48"/></counts>
</article-meta>
</front>
<body/>
<back>
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