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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" specific-use="SMUR" dtd-version="3.0" xml:lang="en">
<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>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys. Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-10-28183-2010</article-id>
<title-group>
<article-title>The impact of different nitrous acid sources in the air quality levels of the Iberian Peninsula</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Gonçalves</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Dabdub</surname>
<given-names>D.</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>Chang</surname>
<given-names>W. L.</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>Saiz</surname>
<given-names>F.</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>Jorba</surname>
<given-names>O.</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>Baldasano</surname>
<given-names>J. M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Environmental Modeling Laboratory, Projects Department, Technical University of Catalonia, Barcelona, Spain</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Earth Sciences Department, Barcelona Supercomputing Center, Barcelona, Spain</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Mechanical and Aerospace Engineering, University of California, Irvine, Irvine, California, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>17</day>
<month>11</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>11</issue>
<fpage>28183</fpage>
<lpage>28230</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2010 M. Gonçalves et al.</copyright-statement>
<copyright-year>2010</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://acp.copernicus.org/preprints/10/28183/2010/acpd-10-28183-2010.html">This article is available from https://acp.copernicus.org/preprints/10/28183/2010/acpd-10-28183-2010.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/preprints/10/28183/2010/acpd-10-28183-2010.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/preprints/10/28183/2010/acpd-10-28183-2010.pdf</self-uri>
<abstract>
<p>Hydroxyl radical (OH) is a primary oxidant in the atmosphere and affects
both gas-phase pollutants and particulate matter levels. Nitrous acid (HONO)
acts as an important source of OH in the urban atmosphere. Therefore it is
important to account accurately for HONO sources within air quality models
in order to predict air pollution dynamics. HONO observations in urban areas
are characterized by high concentrations at night and low concentrations
around midday. Existing gas-phase chemical mechanisms do not reproduce the
observed HONO levels, suggesting a lack of sources, such as direct emissions
or heterogeneous reactions. Specific HONO emission rates, heterogeneous
chemical mechanisms leading to its formation and related kinetics are still
unclear. Therefore, most air quality models consider exclusively gas-phase
chemistry related to HONO. This work applies the WRF-ARW/HERMES/CMAQ
modeling system to quantify the effect of the addition of HONO sources in
the predictability of HONO profiles, and its subsequent effect on secondary
pollutants formation (mainly O&lt;sub&gt;3&lt;/sub&gt; and PM&lt;sub&gt;2.5&lt;/sub&gt;). The modeling episode
is based on a 2004 severe summertime pollution event in the Iberian
Peninsula, using high resolution of 4 × 4 km&lt;sup&gt;2&lt;/sup&gt;. Two different
parameterizations for emissions and the hydrolysis of NO&lt;sub&gt;2&lt;/sub&gt; on wet
surfaces are added as HONO sources in the atmosphere. Emissions have the
largest impact on HONO levels, especially in urban areas, where they can
contribute from 66% to 94% to the HONO peak concentration.
Additionally, in urban environments, NO&lt;sub&gt;2&lt;/sub&gt; hydrolysis on building and
vegetation surfaces contributes up to 30% to the HONO peak. Both, the
available surface area and the relative humidity must be included as
parameters affecting the NO&lt;sub&gt;2&lt;/sub&gt; hydrolysis kinetics. As a result, NO&lt;sub&gt;2&lt;/sub&gt;
hydrolysis is negligible on aerosol surfaces, due to the small surface area
available for reaction, and it is more effective in producing HONO below
high relative humidity conditions. The addition of HONO sources affects the
concentration of secondary pollutants. In particular, major changes are
produced in the early morning, due to the higher OH release via HONO
photolysis. Significant changes in PM&lt;sub&gt;2.5&lt;/sub&gt; concentrations are predicted,
that can be 16% (2.6 μg m&lt;sup&gt;−3&lt;/sup&gt;) higher in the new scenarios. When
accounting for HONO sources, nitrate levels increase especially in urban
areas and sulfates in areas downwind from conventional power plants in the
Iberian Peninsula. Also, O&lt;sub&gt;3&lt;/sub&gt; peak concentrations are slightly affected
(from 0.7 to 4 ppb, 1% to 4.5%). The improvement of the HONO sources
representation within air quality models produces changes in O&lt;sub&gt;3&lt;/sub&gt; peak
predictions and significantly affects the reaction pathways leading to
aerosols formation. Therefore, HONO sources other than gas-phase chemistry
should be accurately included within modeling frameworks.</p>
</abstract>
<counts><page-count count="48"/></counts>
</article-meta>
</front>
<body/>
<back>
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