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<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>
</journal-title-group>
<issn pub-type="epub">1680-7375</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/acpd-9-81-2009</article-id>
<title-group>
<article-title>Quantitative long-term measurements of VOC concentrations by PTR-MS: annual  cycle at a boreal forest site</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ruuskanen</surname>
<given-names>T. M.</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>Taipale</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>Rinne</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>Kajos</surname>
<given-names>M. 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>Hakola</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>Kulmala</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>University of Helsinki, Department of Physics, P.O. Box 68, 00014 University of Helsinki, Finland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Finnish Meteorological Institute, P.O. Box 503, 00101 Helsinki, Finland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>06</day>
<month>01</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>1</issue>
<fpage>81</fpage>
<lpage>134</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-discuss.net/9/81/2009/acpd-9-81-2009.html">This article is available from http://www.atmos-chem-phys-discuss.net/9/81/2009/acpd-9-81-2009.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/9/81/2009/acpd-9-81-2009.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/9/81/2009/acpd-9-81-2009.pdf</self-uri>
<abstract>
<p>Atmospheric concentrations of volatile organic compounds (VOCs) vary
      diurnally, seasonally and annually. Therefore continuous long-term
      measurements are needed to properly describe the atmospheric levels of
      these chemically reactive compounds. We conducted on-line measurements
      of atmospheric volume mixing ratios of several VOCs in the European
      boreal region with a proton transfer reaction â€“ mass spectrometer
      (PTR-MS) over a 15 month period. The measurements lasted from spring
      2006 to fall 2007 and were conducted at SMEAR II station in
      south-western Finland. The measured compounds included for example
      methanol, acetone, sum of isoprene and 2-methyl-3-buten-2-ol (MBO),
      monoterpenes and benzene. The VOC mixing ratios were measured inside
      and above canopy, during every second or third hour. The PTR-MS was
      calibrated regularly and background signals of VOCs were measured
      every second or third hour from the zero air and subtracted from the
      measured volume mixing ratio. In the continuous measurements at
      moderate VOC mixing ratios we observed that the PTR-MS has to be
      calibrated and SEM operation voltage checked regularly, at least twice
      a month to ensure reliable measurements. Of the measured VOCs,
      methanol and acetone were the most abundant ones, their volume mixing
      ratio medians were in the order of 1 ppbv. Volume mixing
      ratios of methanol, acetone, isoprene-MBO and monoterpenes were high
      during summer and low in winter indicating mostly biogenic or
      photochemical local or regional origin. Benzene behaved in the
      opposite way, while seasonal variation of acetaldehyde and
      methacrolein-methylvinylketone (MACR-MVK) was less profound. Methanol,
      acetone, isoprene and monoterpene volume mixing ratios had clear
      diurnal patterns during summers, while the mixing ratios of other VOCs
      did not exhibit this behavior. During winter we did not observe
      systematic diurnal cycles in the VOC volume mixing ratios.</p>
</abstract>
<counts><page-count count="54"/></counts>
</article-meta>
</front>
<body/>
<back>
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