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<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" dtd-version="3.0" xml:lang="en">
<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-10-6283-2010</article-id>
<title-group>
<article-title>Measurement of atmospheric nitrous acid at Bodgett Forest during BEARPEX2007</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ren</surname>
<given-names>X.</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>Gao</surname>
<given-names>H.</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>Zhou</surname>
<given-names>X.</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>Crounse</surname>
<given-names>J. D.</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>Wennberg</surname>
<given-names>P. O.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Browne</surname>
<given-names>E. C.</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>LaFranchi</surname>
<given-names>B. W.</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
<xref ref-type="aff" rid="aff11">
<sup>11</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="aff7">
<sup>7</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>McKay</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
<xref ref-type="aff" rid="aff12">
<sup>12</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Goldstein</surname>
<given-names>A. H.</given-names>
</name>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Mao</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff10">
<sup>10</sup>
</xref>
<xref ref-type="aff" rid="aff13">
<sup>13</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, FL, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Environmental Health Sciences, State University of New York at Albany, Albany, NY, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Wadsworth Center, New York State Department of Health, Albany, NY, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Division of Engineering and Applied Sciences, California Institute of Technology, Pasadena, CA, USA</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA, USA</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>Department of Chemistry, University of California at Berkeley, Berkeley, CA, USA</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>Department of Earth and Planetary Science, University of California at Berkeley, Berkeley, CA, USA</addr-line>
</aff>
<aff id="aff9">
<label>9</label>
<addr-line>Department of Environmental Science, Policy, and Management, University of California at Berkeley, Berkeley, CA, USA</addr-line>
</aff>
<aff id="aff10">
<label>10</label>
<addr-line>Department of Meteorology, Pennsylvania State University, University Park, PA, USA</addr-line>
</aff>
<aff id="aff11">
<label>11</label>
<addr-line>now at: Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, Livermore, CA, USA</addr-line>
</aff>
<aff id="aff12">
<label>12</label>
<addr-line>now at: California Air Resources Board, Sacramento, CA, USA</addr-line>
</aff>
<aff id="aff13">
<label>13</label>
<addr-line>now at: School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>12</day>
<month>07</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>13</issue>
<fpage>6283</fpage>
<lpage>6294</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/10/6283/2010/acp-10-6283-2010.html">This article is available from http://www.atmos-chem-phys.net/10/6283/2010/acp-10-6283-2010.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/10/6283/2010/acp-10-6283-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/10/6283/2010/acp-10-6283-2010.pdf</self-uri>
<abstract>
<p>Nitrous acid (HONO) is an important precursor of the hydroxyl radical (OH)
in the lower troposphere. Understanding HONO chemistry, particularly its
sources and contribution to HO&lt;sub&gt;x&lt;/sub&gt; (=OH+HO&lt;sub&gt;2&lt;/sub&gt;) production, is very
important for understanding atmospheric oxidation processes. A highly
sensitive instrument for detecting atmospheric HONO based on wet chemistry
followed by liquid waveguide long path absorption photometry was deployed in
the Biosphere Effects on Aerosols and Photochemistry Experiment (BEARPEX) at
Blodgett Forest, California in late summer 2007. The median diurnal
variation shows minimum HONO levels of about 20â€“30 pptv during the day and
maximum levels of about 60â€“70 pptv at night, a diurnal pattern quite
different from the results at various other forested sites. Measured
HONO/NO&lt;sub&gt;2&lt;/sub&gt; ratios for a 24-h period ranged from 0.05 to 0.13 with a
mean ratio of 0.07. Speciation of reactive nitrogen compounds (NO&lt;sub&gt;y&lt;/sub&gt;)
indicates that HONO accounted for only ~3% of total NO&lt;sub&gt;y&lt;/sub&gt;.
However, due to the fast HONO loss through photolysis, a strong HONO source
(1.59 ppbv day&lt;sup&gt;âˆ’1&lt;/sup&gt;) existed in this environment in order to sustain the
observed HONO levels, indicating the significant role of HONO in NO&lt;sub&gt;y&lt;/sub&gt;
cycling. The wet chemistry HONO measurements were compared to the HONO
measurements made with a Chemical Ionization Mass Spectrometer (CIMS) over a
three-day period. Good agreement was obtained between the measurements from
the two different techniques. Using the expansive suite of photochemical and
meteorological measurements, the contribution of HONO photolysis to HO&lt;sub&gt;x&lt;/sub&gt;
budget was calculated to be relatively small (6%) compared to results
from other forested sites. The lower HONO mixing ratio and thus its smaller
contribution to HO&lt;sub&gt;x&lt;/sub&gt; production are attributed to the unique
meteorological conditions and low acid precipitation at Blodgett Forest.
Further studies of HONO in this kind of environment are needed to test this
hypothesis and to improve our understanding of atmospheric oxidation and
nitrogen budget.</p>
</abstract>
<counts><page-count count="12"/></counts>
</article-meta>
</front>
<body/>
<back>
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