<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "http://dtd.nlm.nih.gov/publishing/3.0/journalpublishing3.dtd">
<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>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-4-215-2004</article-id>
<title-group>
<article-title>Tethered balloon measurements of biogenic volatile organic compounds at a Boreal forest site</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Spirig</surname>
<given-names>C.</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>Guenther</surname>
<given-names>A.</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>Greenberg</surname>
<given-names>J. P.</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>Calanca</surname>
<given-names>P.</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>Tarvainen</surname>
<given-names>V.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Swiss Federal Research Station for Agroecology and Agriculture, Zürich, Switzerland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>National Center for Atmospheric Research, Boulder, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Finnish Meteorological Institute, Helsinki, Finland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>06</day>
<month>02</month>
<year>2004</year>
</pub-date>
<volume>4</volume>
<issue>1</issue>
<fpage>215</fpage>
<lpage>229</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/4/215/2004/acp-4-215-2004.html">This article is available from http://www.atmos-chem-phys.net/4/215/2004/acp-4-215-2004.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/4/215/2004/acp-4-215-2004.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/4/215/2004/acp-4-215-2004.pdf</self-uri>
<abstract>
<p>Measurements of biogenic volatile organic compounds
      (VOCs) were performed at Hyytiälä, a Boreal forest site in Southern Finland as part of the
      OSOA (origin and formation of secondary organic aerosol) project in August
      2001. At this site, frequent formation of new particles has been observed and the role of biogenic VOCs in this process is still unclear. Tethered
      balloons served as platforms to collect VOC samples within the planetary boundary layer at heights up to
      1.2 km above ground during daytime. Mean mixed layer concentrations of total monoterpenes varied between 10 and
      170 pptv, with &lt;font face=&quot;Symbol&quot;&gt;a&lt;/font&gt;-pinene, limonene and
      &lt;font face=&quot;Symbol&quot;&gt;D&lt;/font&gt;&lt;sup&gt;3&lt;/sup&gt;-carene as major
      compounds, isoprene was detected at levels of 2-35 pptv. A mixed layer gradient technique and a budget approach are applied to derive surface
      fluxes representative for areas of tens to hundreds of square kilometres. Effects of spatial heterogeneity in surface emissions are examined with a
      footprint analysis. Depending on the source area considered, mean afternoon
      emissions of the sum of terpenes range between 180 and 300 &lt;font face=&quot;Symbol&quot;&gt;m&lt;/font&gt;g
      m&lt;sup&gt;-2&lt;/sup&gt; h&lt;sup&gt;-1&lt;/sup&gt; for the period of 2-12 August 2001. Surface fluxes close to
      Hyytiälä were higher than the regional average, and agree well with mean emissions predicted by a biogenic VOC emission model. Total rates of
      monoterpene oxidation were calculated with a photochemical model. The rates
      did not correlate with the occurrence of new particle formation, but the ozone pathway was of more importance on days with particle formation.
      Condensable vapour production from the oxidation of monoterpenes throughout
      the mixed layer can only account for a fraction of the increase in aerosol
      mass observed at the surface.</p>
</abstract>
<counts><page-count count="15"/></counts>
</article-meta>
</front>
<body/>
<back>
</back>
</article>