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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-11-6425-2011</article-id>
<title-group>
<article-title>H&lt;sub&gt;2&lt;/sub&gt; vertical profiles in the continental boundary layer: measurements at the Cabauw tall tower in The Netherlands</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Popa</surname>
<given-names>M. E.</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>Vermeulen</surname>
<given-names>A. T.</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>van den Bulk</surname>
<given-names>W. C. 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>Jongejan</surname>
<given-names>P. A. C.</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>Batenburg</surname>
<given-names>A. M.</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>Zahorowski</surname>
<given-names>W.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Röckmann</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Energy research Centre of the Netherlands, Petten, The Netherlands</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute for Marine and Atmospheric Research Utrecht, Utrecht University, Utrecht, The Netherlands</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Australian Nuclear Science and Technology Organisation, Menai, New South Wales, Australia</addr-line>
</aff>
<pub-date pub-type="epub">
<day>06</day>
<month>07</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>13</issue>
<fpage>6425</fpage>
<lpage>6443</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/11/6425/2011/acp-11-6425-2011.html">This article is available from http://www.atmos-chem-phys.net/11/6425/2011/acp-11-6425-2011.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/6425/2011/acp-11-6425-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/6425/2011/acp-11-6425-2011.pdf</self-uri>
<abstract>
<p>In-situ, quasi-continuous measurements of atmospheric hydrogen (H&lt;sub&gt;2&lt;/sub&gt;)
have been performed since October 2007 at the Cabauw tall tower station in
the Netherlands. Mole fractions of H&lt;sub&gt;2&lt;/sub&gt;, CO and several greenhouse gases
are determined simultaneously in air sampled successively at four heights,
between 20 and 200 m above ground level. &lt;sup&gt;222&lt;/sup&gt;Rn measurements are
performed in air sampled at 20 and 200 m.
&lt;br&gt;&lt;/br&gt;
This H&lt;sub&gt;2&lt;/sub&gt; dataset represents the first in-situ, quasi-continuous
long-term measurement series of vertical profiles of H&lt;sub&gt;2&lt;/sub&gt; in the lower
continental boundary layer. Seasonal cycles are present at all heights in
both H&lt;sub&gt;2&lt;/sub&gt; and CO, and their amplitude varies with the sampling height.
The seasonality is evident in both the &quot;baseline&quot; values and in the short
term (diurnal to synoptic time scales) variability, the latter being
significantly larger during winter.
&lt;br&gt;&lt;/br&gt;
The observed H&lt;sub&gt;2&lt;/sub&gt; short term signals and vertical gradients are in many
cases well correlated to other species, especially to CO. On the other hand,
H&lt;sub&gt;2&lt;/sub&gt; has at times a unique behaviour, due to its particular distribution
of sources and sinks.
&lt;br&gt;&lt;/br&gt;
Our estimation for the regional H&lt;sub&gt;2&lt;/sub&gt; soil uptake flux, using the radon
tracer method, is (&amp;minus;1.89 ± 0.26) &amp;times; 10&lt;sup&gt;&amp;minus;5&lt;/sup&gt; g/(m&lt;sup&gt;2&lt;/sup&gt; h),
significantly smaller than other recent results from Europe.
&lt;br&gt;&lt;/br&gt;
H&lt;sub&gt;2&lt;/sub&gt;/CO ratios of the traffic emissions computed from our data, with an
average of 0.54 ± 0.07 mol:mol, are larger and more variable than
estimated in some of the previous studies in Europe. This difference can be
explained by a different driving regime, due to the frequent traffic jams in
the influence area of Cabauw. The H&lt;sub&gt;2&lt;/sub&gt;/CO ratios of the large scale
pollution events have an average of 0.36 ± 0.05 mol:mol; these ratios
were observed to slightly increase with sampling height, possibly due to a
stronger influence of soil uptake at the lower sampling heights.</p>
</abstract>
<counts><page-count count="19"/></counts>
</article-meta>
</front>
<body/>
<back>
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