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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-9-9369-2009</article-id>
<title-group>
<article-title>Methane and nitrous oxide emissions in The Netherlands: ambient measurements support the national inventories</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>van der Laan</surname>
<given-names>S.</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>Neubert</surname>
<given-names>R. E. 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>Meijer</surname>
<given-names>H. A. J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Centre for Isotope Research, University of Groningen, Groningen, The Netherlands</addr-line>
</aff>
<pub-date pub-type="epub">
<day>15</day>
<month>12</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>24</issue>
<fpage>9369</fpage>
<lpage>9379</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2009 S. van der Laan et al.</copyright-statement>
<copyright-year>2009</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/9/9369/2009/acp-9-9369-2009.html">This article is available from https://acp.copernicus.org/articles/9/9369/2009/acp-9-9369-2009.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/9/9369/2009/acp-9-9369-2009.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/9/9369/2009/acp-9-9369-2009.pdf</self-uri>
<abstract>
<p>We present net emission estimates of CH&lt;sub&gt;4&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O of The
Netherlands based on measurements conducted during the period of May 2006 to
April 2009 at station Lutjewad, The Netherlands (6&amp;deg;21&apos; E,
53&amp;deg;24&apos; N, 1 m a.s.l.). &lt;sup&gt;222&lt;/sup&gt;Radon mixing ratios were applied as an indicator
for vertical mixing and long-range air mass transport and used to calculate
the net surface fluxes from atmospheric mixing ratios of CH&lt;sub&gt;4&lt;/sub&gt; and
N&lt;sub&gt;2&lt;/sub&gt;O. Our study shows that our measurement site Lutjewad is well-suited
to measure emissions from The Netherlands and validation of the national
inventories using the &lt;sup&gt;222&lt;/sup&gt;Radon flux method. Since this study is purely
observation-based it is independent from inventories or atmospheric models.
Our results are compared to the national inventories as reported to the
UNFCCC. We found net emissions of: (15.2&amp;plusmn;5.3) t km&lt;sup&gt;&amp;minus;2&lt;/sup&gt; a&lt;sup&gt;&amp;minus;1&lt;/sup&gt; for
CH&lt;sub&gt;4&lt;/sub&gt; and (0.9&amp;plusmn;0.3) t km&lt;sup&gt;&amp;minus;2&lt;/sup&gt; a&lt;sup&gt;&amp;minus;1&lt;/sup&gt; for N&lt;sub&gt;2&lt;/sub&gt;O. These values
are lower than the inventory-based emissions (2006-2008 averages) of
(18.3&amp;plusmn;3.3) t km&lt;sup&gt;&amp;minus;2&lt;/sup&gt; a&lt;sup&gt;&amp;minus;1&lt;/sup&gt; for CH&lt;sub&gt;4&lt;/sub&gt;, and
(1.3&amp;plusmn;0.6) t km&lt;sup&gt;&amp;minus;2&lt;/sup&gt; a&lt;sup&gt;&amp;minus;1&lt;/sup&gt; for N&lt;sub&gt;2&lt;/sub&gt;O, but
the differences are insignificant.</p>
</abstract>
<counts><page-count count="11"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>