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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>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-12-1923-2012</article-id>
<title-group>
<article-title>Coupling processes and exchange of energy and reactive and non-reactive trace gases at a forest site – results of the EGER experiment</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Foken</surname>
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<sup>1</sup>
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<sup>5</sup>
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<sup>2</sup>
</xref>
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<given-names>E.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
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<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
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<sup>5</sup>
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<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
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<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
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</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
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</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
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<xref ref-type="aff" rid="aff1">
<sup>1</sup>
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</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
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</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
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<xref ref-type="aff" rid="aff6">
<sup>6</sup>
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<xref ref-type="aff" rid="aff2">
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</name>
<xref ref-type="aff" rid="aff2">
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<xref ref-type="aff" rid="aff2">
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<xref ref-type="aff" rid="aff1">
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<xref ref-type="aff" rid="aff3">
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</name>
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</name>
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<xref ref-type="aff" rid="aff2">
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<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zhu</surname>
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</name>
<xref ref-type="aff" rid="aff2">
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</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>University of Bayreuth, Department of Micrometeorology, 95440 Bayreuth, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Max-Planck-Institute of Chemistry, Biogeochemistry Department, P.O. Box 3060, 55020 Mainz, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>University of Bayreuth, Atmospheric Chemistry Research Laboratory, 95440 Bayreuth, Germany</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>University of Zimbabwe, Department of Physics, P.O. Box MP 167, Mount Pleasant, Harare, Zimbabwe</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Member of Bayreuth Center of Ecology and Environmental Research (BayCEER), University of Bayreuth, 95440 Bayreuth, Germany</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>now at: TÜV Süd Industrie Service GmbH Wind Cert Services, Ludwig-Eckert-Straße 10, 93049 Regensburg, Germany</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>now at: Alfred-Wegener Institute for Polar and Marine Research, Telegrafenberg A43, 14473 Potsdam, Germany</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>now at: German Aerospace Center (DLR), Institute of Atmospheric Physics, Münchner Straße 20, 82234 Oberpfaffenhofen-Wessling, Germany</addr-line>
</aff>
<aff id="aff9">
<label>9</label>
<addr-line>now at: Institut National de la Recherche Agronomique (INRA), BP 709, 97387 Cedex Kourou, French Guiana</addr-line>
</aff>
<aff id="aff10">
<label>10</label>
<addr-line>now at: Agroscope ART Research Station, Reckenholzstrasse 191, 8046 Zürich, Switzerland</addr-line>
</aff>
<aff id="aff11">
<label>11</label>
<addr-line>now at: Institute for Geographic Sciences and Natural Resources Research, ChineseAcademy of Sciences (CAS), A11 Datun Road, Anwai, Beijing 100101, China</addr-line>
</aff>
<pub-date pub-type="epub">
<day>17</day>
<month>02</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>4</issue>
<fpage>1923</fpage>
<lpage>1950</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2012 T. Foken et al.</copyright-statement>
<copyright-year>2012</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/articles/12/1923/2012/acp-12-1923-2012.html">This article is available from https://acp.copernicus.org/articles/12/1923/2012/acp-12-1923-2012.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/12/1923/2012/acp-12-1923-2012.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/12/1923/2012/acp-12-1923-2012.pdf</self-uri>
<abstract>
<p>To investigate the energy, matter and reactive and non-reactive trace gas
exchange between the atmosphere and a spruce forest in the German mountain
region, two intensive measuring periods were conducted at the FLUXNET site
DE-Bay (&lt;i&gt;Waldstein-Weidenbrunnen&lt;/i&gt;) in September/October 2007 and June/July 2008. They were part of the
project &quot;ExchanGE processes in mountainous Regions&quot; (EGER). Beyond a brief
description of the experiment, the main focus of the paper concerns the
coupling between the trunk space, the canopy and the above-canopy
atmosphere. Therefore, relevant coherent structures were analyzed for
different in- and above canopy layers, coupling between layers was
classified according to already published procedures, and gradients and
fluxes of meteorological quantities as well as concentrations of
non-reactive and reactive trace compounds have been sorted along the
coupling classes. Only in the case of a fully coupled system, it could be
shown, that fluxes measured above the canopy are related to gradients
between the canopy and the above-canopy atmosphere. Temporal changes of
concentration differences between top of canopy and the forest floor,
particularly those of reactive trace gases (NO, NO&lt;sub&gt;2&lt;/sub&gt;, O&lt;sub&gt;3&lt;/sub&gt;, and HONO)
could only be interpreted on the basis of the coupling stage. Consequently,
only concurrent and vertically resolved measurements of micrometeorological
(turbulence) quantities and fluxes (gradients) of trace compounds will lead
to a better understanding of the forest-atmosphere interaction.</p>
</abstract>
<counts><page-count count="28"/></counts>
</article-meta>
</front>
<body/>
<back>
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