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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>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-9-8283-2009</article-id>
<title-group>
<article-title>Observations of heterogeneous reactions between Asian pollution and mineral dust over the Eastern North Pacific during INTEX-B</article-title>
</title-group>
<contrib-group><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="aff1">
<sup>1</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="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kapustin</surname>
<given-names>V.</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>Shinozuka</surname>
<given-names>Y.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff9">
<sup>9</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="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Anderson</surname>
<given-names>B. E.</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>Winstead</surname>
<given-names>E.</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>Dibb</surname>
<given-names>J.</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>Scheuer</surname>
<given-names>E.</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>Cohen</surname>
<given-names>R. C.</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>Wooldridge</surname>
<given-names>P.</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>Perring</surname>
<given-names>A.</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>Huey</surname>
<given-names>L. 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>Kim</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>Jimenez</surname>
<given-names>J. L.</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>Dunlea</surname>
<given-names>E. J.</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>DeCarlo</surname>
<given-names>P. F.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
<xref ref-type="aff" rid="aff10">
<sup>10</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wennberg</surname>
<given-names>P. O.</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>Crounse</surname>
<given-names>J. D.</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>Weinheimer</surname>
<given-names>A. J.</given-names>
</name>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Flocke</surname>
<given-names>F.</given-names>
</name>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>School of Ocean and Earth Science and Technology, University of Hawaii, Honolulu, 96822 HI, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>NASA Langley Research Center, Hampton, 23665 VA, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>University of New Hampshire, Durham, 03824 NH, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>University of California Berkeley, Berkeley, 94720 CA, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Georgia Institute of Technology, Atlanta, 30332 GA, USA</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Cooperative Institute for Research in Environmental Sciences (CIRES) and University of Colorado, Boulder, 80309 CO, USA</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>California Institute of Technology, Pasadena, 91125 CA, USA</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>National Center for Atmospheric Research, Boulder, 80307 CO, USA</addr-line>
</aff>
<aff id="aff9">
<label>9</label>
<addr-line>now at: NASA Ames Research Center, Moffett Field, 94035 CA, USA</addr-line>
</aff>
<aff id="aff10">
<label>10</label>
<addr-line>now at: Paul Scherrer Institute, 5232 Villigen-PSI, Switzerland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>03</day>
<month>11</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>21</issue>
<fpage>8283</fpage>
<lpage>8308</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/9/8283/2009/acp-9-8283-2009.html">This article is available from http://www.atmos-chem-phys.net/9/8283/2009/acp-9-8283-2009.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/9/8283/2009/acp-9-8283-2009.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/9/8283/2009/acp-9-8283-2009.pdf</self-uri>
<abstract>
<p>In-situ airborne measurements of trace gases, aerosol size distributions,
chemistry and optical properties were conducted over Mexico and the Eastern
North Pacific during MILAGRO and INTEX-B. Heterogeneous reactions between
secondary aerosol precursor gases and mineral dust lead to sequestration of
sulfur, nitrogen and chlorine in the supermicrometer particulate size range.
&lt;br&gt;&lt;br&gt;
Simultaneous measurements of aerosol size distributions and weak-acid
soluble calcium result in an estimate of 11 wt% of CaCO&lt;sub&gt;3&lt;/sub&gt; for Asian
dust. During transport across the North Pacific, ~5â€“30% of the
CaCO&lt;sub&gt;3&lt;/sub&gt; is converted to CaSO&lt;sub&gt;4&lt;/sub&gt; or Ca(NO&lt;sub&gt;3&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt; with an
additional ~4% consumed through reactions with HCl. The 1996 to
2008 record from the Mauna Loa Observatory confirm these findings,
indicating that, on average, 19% of the CaCO&lt;sub&gt;3&lt;/sub&gt; has reacted to form
CaSO&lt;sub&gt;4&lt;/sub&gt; and 7% has reacted to form Ca(NO&lt;sub&gt;3&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt; and ~2%
has reacted with HCl. In the nitrogen-oxide rich boundary layer near Mexico
City up to 30% of the CaCO&lt;sub&gt;3&lt;/sub&gt; has reacted to form Ca(NO&lt;sub&gt;3&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;
while an additional 8% has reacted with HCl.
&lt;br&gt;&lt;br&gt;
These heterogeneous reactions can result in a ~3% increase in dust
solubility which has an insignificant effect on their optical properties
compared to their variability in-situ. However, competition between
supermicrometer dust and submicrometer primary aerosol for condensing
secondary aerosol species led to a 25% smaller number median diameter for
the accumulation mode aerosol. A 10â€“25% reduction of accumulation mode
number median diameter results in a 30â€“70% reduction in submicrometer
light scattering at relative humidities in the 80â€“95% range. At 80% RH
submicrometer light scattering is only reduced ~3% due to a higher
mass fraction of hydrophobic refractory components in the dust-affected
accumulation mode aerosol. Thus reducing the geometric mean diameter of the
submicrometer aerosol has a much larger effect on aerosol optical properties
than changes to the hygroscopic:hydrophobic mass fractions of the
accumulation mode aerosol.
&lt;br&gt;&lt;br&gt;
In the presence of dust, nitric acid concentrations are reduced to &lt;50%
of total nitrate (nitric acid plus particulate nitrate). NO&lt;sub&gt;y&lt;/sub&gt; as a
fraction of total nitrogen (NO&lt;sub&gt;y&lt;/sub&gt; plus particulate nitrate), is reduced
from &gt;85% to 60â€“80% in the presence of dust. These observations
support previous model studies which predict irreversible sequestration of
reactive nitrogen species through heterogeneous reactions with mineral dust
during long-range transport.</p>
</abstract>
<counts><page-count count="26"/></counts>
</article-meta>
</front>
<body/>
<back>
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