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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-8-6823-2008</article-id>
<title-group>
<article-title>Measurements of HNO&lt;sub&gt;3&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; using ion drift-chemical ionization mass spectrometry during the MILAGRO/MCMA-2006 campaign</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zheng</surname>
<given-names>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>Zhang</surname>
<given-names>R.</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>Fortner</surname>
<given-names>E. C.</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>Volkamer</surname>
<given-names>R. M.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</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>Molina</surname>
<given-names>L.</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>Aiken</surname>
<given-names>A. C.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</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="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Gaeggeler</surname>
<given-names>K.</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>Dommen</surname>
<given-names>J.</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>Dusanter</surname>
<given-names>S.</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>Stevens</surname>
<given-names>P. S.</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>Tie</surname>
<given-names>X.</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Dept. of Atmospheric Sciences, Texas A&amp;M University, College Station, Texas 77843, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Molina Center for Energy and the Environment, La Jolla, California and Massachusetts Institute of Technology, Cambridge, Massachusetts, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Dept. of Chemistry and Biochemistry, University of Colorado at Boulder, Boulder CO, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Cooperative Institute for Research in the Environmental Sciences (CIRES), University of Colorado, Boulder, Colorado, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Switzerland</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Dept. of Chemistry, Indiana University, Bloomington, Indiana, USA</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>Atmospheric Chemistry Division, National Center for Atmospheric Research, Boulder, Colorado, USA</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>now at: Dept. of Chemistry and Biochemistry, Montana State University, Bozeman, Montana, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>28</day>
<month>11</month>
<year>2008</year>
</pub-date>
<volume>8</volume>
<issue>22</issue>
<fpage>6823</fpage>
<lpage>6838</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/8/6823/2008/acp-8-6823-2008.html">This article is available from http://www.atmos-chem-phys.net/8/6823/2008/acp-8-6823-2008.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/8/6823/2008/acp-8-6823-2008.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/8/6823/2008/acp-8-6823-2008.pdf</self-uri>
<abstract>
<p>An ion drift-chemical ionization mass spectrometer (ID-CIMS) was deployed in
Mexico City between 7 and 31 March to measure gas-phase nitric acid
(HNO&lt;sub&gt;3&lt;/sub&gt;) and dinitrogen pentoxide (N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; during the Mexico City
Metropolitan Area (MCMA)-2006 field campaign. The observation site was
located at the Instituto Mexicano del Petróleo in the northern part of
Mexico City urban area with major emissions of pollutants from residential,
vehicular and industrial sources. Diurnally, HNO&lt;sub&gt;3&lt;/sub&gt; was less than 200
parts per trillion (ppt) during the night and early morning. The
concentration of HNO&lt;sub&gt;3&lt;/sub&gt; increased steadily from around 09:00 a.m. central
standard time (CST), reached a peak value of 0.5 to 3 parts per billion (ppb)
in the early afternoon, and then declined sharply to less than half of the
peak value near 05:00 p.m. CST. An inter-comparison between the ID-CIMS and
an ion chromatograph/mass spectrometer (ICMS) showed a good agreement between
the two HNO&lt;sub&gt;3&lt;/sub&gt; measurements (&lt;i&gt;R&lt;/i&gt;&lt;sup&gt;2&lt;/sup&gt;=0.75). The HNO&lt;sub&gt;3&lt;/sub&gt; mixing ratio
was found to anti-correlate with submicron-sized aerosol nitrate, suggesting
that the gas-particle partitioning process was a major factor in determining
the gaseous HNO&lt;sub&gt;3&lt;/sub&gt; concentration. Losses by irreversible reactions with
mineral dust and via dry deposition also could be important at this site.
Most of the times during the MCMA 2006 field campaign, N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; was
found to be below the detection limit (about 30 ppt for a 10 s integration
time) of the ID-CIMS, because of high NO mixing ratio at the surface
(&amp;gt;100 ppb) during the night. An exception occurred on 26 March 2006, when
about 40 ppt N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; was observed during the late afternoon and
early evening hours under cloudy conditions before the build-up of NO at the
surface site. The results revealed that during the MCMA-2006 field campaign
HNO&lt;sub&gt;3&lt;/sub&gt; was primarily produced from the reaction of OH with NO&lt;sub&gt;2&lt;/sub&gt; and
regulated by gas/particle transfer and dry deposition. The production of
HNO&lt;sub&gt;3&lt;/sub&gt; from N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; hydrolysis during the nighttime was small
because of high NO and low O&lt;sub&gt;3&lt;/sub&gt; concentrations near the surface.</p>
</abstract>
<counts><page-count count="16"/></counts>
</article-meta>
</front>
<body/>
<back>
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