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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-4-1265-2004</article-id>
<title-group>
<article-title>Assessment of the applicability of NO-NO&lt;sub&gt;2&lt;/sub&gt;-O&lt;sub&gt;3&lt;/sub&gt; photostationary state to long-term measurements at the Hohenpeissenberg GAW Station, Germany</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Mannschreck</surname>
<given-names>K.</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>Gilge</surname>
<given-names>S.</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>Plass-Duelmer</surname>
<given-names>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>Fricke</surname>
<given-names>W.</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>Berresheim</surname>
<given-names>H.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Umweltforschungsstation Schneefernerhaus, Zugspitze, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Deutscher Wetterdienst, Meteorologisches Observatorium Hohenpeissenberg, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>17</day>
<month>08</month>
<year>2004</year>
</pub-date>
<volume>4</volume>
<issue>5</issue>
<fpage>1265</fpage>
<lpage>1277</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/4/1265/2004/acp-4-1265-2004.html">This article is available from http://www.atmos-chem-phys.net/4/1265/2004/acp-4-1265-2004.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/4/1265/2004/acp-4-1265-2004.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/4/1265/2004/acp-4-1265-2004.pdf</self-uri>
<abstract>
<p>Continuous measurements of concentrations of reactive gases, radiation, and
meteorological parameters are carried out at the Meteorological Observatory
Hohenpeissenberg (MOHp) as part of the Global Atmosphere Watch (GAW)
Program. NO, NO&lt;sub&gt;2&lt;/sub&gt;, O&lt;sub&gt;3&lt;/sub&gt; and J&lt;sub&gt;NO2&lt;/sub&gt; data from a four-year period
(March 1999-December 2002) are evaluated for consistency with
photochemical steady state (PSS, &amp;Phi;=1) conditions. The extent
of deviation from PSS reveals a strong dependence on wind direction at the
station. Median values of &amp;Phi; in the south sector are in the range of
2.5-5.7 and show a high variability. In contrast, values for the other
directions show a relatively low variability around a median level of 2.
When taking into account peroxy radical concentrations (&amp;Phi;&lt;sub&gt;ext&lt;/sub&gt;=1)
PSS was reached in 13-32% of all cases for the years 1999-2002.

&lt;P  style=&quot;line-height: 20px;&quot;&gt;
The differences in wind sectors can be explained by local effects. It is
shown that the height of the sample inlet line, its distance to the forest
and the surrounding topography has a strong impact on both the absolute and
relative deviations from PSS. Global irradiance and thus, photolysis of
NO&lt;sub&gt;2&lt;/sub&gt; is reduced within the dense forest. Since the reaction of NO with
O&lt;sub&gt;3&lt;/sub&gt; is still proceeding under these conditions, increased NO&lt;sub&gt;2&lt;/sub&gt;/NO
ratios are produced locally in air which is transported through the forest
and advected to the MOHp site.

&lt;P  style=&quot;line-height: 20px;&quot;&gt;
Estimates of the peroxy radical concentration (RO&lt;sub&gt;2&lt;/sub&gt;) inferred from PSS
are compared with peroxy radical measurements made at the site in June 2000
during a three-week campaign. The PSS derived RO&lt;sub&gt;2&lt;/sub&gt; levels were higher
than corresponding measured levels by at least a factor of 2-3. This
analysis was made for a wind sector with minimal local effects on PSS. Thus
the corresponding &amp;Phi; median of 2 can be regarded as an upper limit for
a deviation from PSS due to chemical reactions, i.e. by peroxy radicals and
possible other oxidants converting additional NO to NO&lt;sub&gt;2&lt;/sub&gt;.</p>
</abstract>
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