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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-10-10359-2010</article-id>
<title-group>
<article-title>Review and parameterisation of bi-directional ammonia exchange between vegetation and the atmosphere</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Massad</surname>
<given-names>R.-S.</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>Nemitz</surname>
<given-names>E.</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>Sutton</surname>
<given-names>M. A.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Center for Ecology and Hydrology, Edinburgh Research Station, Bush Estate, Penicuik Midlothian EH26 0QB, UK</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>now at: INRA, AgroParisTech, UMR 1091 EGC, 78850 Thiverval Grignon, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>04</day>
<month>11</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>21</issue>
<fpage>10359</fpage>
<lpage>10386</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/10/10359/2010/acp-10-10359-2010.html">This article is available from http://www.atmos-chem-phys.net/10/10359/2010/acp-10-10359-2010.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/10/10359/2010/acp-10-10359-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/10/10359/2010/acp-10-10359-2010.pdf</self-uri>
<abstract>
<p>Current deposition schemes used in atmospheric chemical transport models do
not generally account for bi-directional exchange of ammonia (NH&lt;sub&gt;3&lt;/sub&gt;).
Bi-directional exchange schemes, which have so far been applied at the plot
scale, can be included in transport models, but need to be parameterised with
appropriate values of the ground layer compensation point (&amp;chi;&lt;sub&gt;g&lt;/sub&gt;),
stomatal compensation point (&amp;chi;&lt;sub&gt;s&lt;/sub&gt;) and cuticular resistance
(&lt;i&gt;R&lt;/i&gt;&lt;sub&gt;w&lt;/sub&gt;). We review existing measurements of &amp;chi;&lt;sub&gt;g&lt;/sub&gt;, &amp;chi;&lt;sub&gt;s&lt;/sub&gt; as well as &lt;i&gt;R&lt;/i&gt;&lt;sub&gt;w&lt;/sub&gt; and compile a comprehensive dataset from which we
then propose generalised parameterisations. &amp;chi;&lt;sub&gt;s&lt;/sub&gt; is related
to &amp;Gamma;&lt;sub&gt;s&lt;/sub&gt;, the non-dimensional ratio of
[NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt;]&lt;sub&gt;apo&lt;/sub&gt; and [H&lt;sup&gt;+&lt;/sup&gt;]&lt;sub&gt;apo&lt;/sub&gt; in the apoplast, through the
temperature dependence of the combined Henry and dissociation equilibrium.
The meta-analysis suggests that the nitrogen (N) input is the main driver of
the apoplastic and bulk leaf concentrations of ammonium (NH&lt;sub&gt;4 apo&lt;/sub&gt;&lt;sup+&lt;/sup&gt;,
NH&lt;sub&gt;4 bulk&lt;/sub&gt;&lt;sup+&lt;/sup&gt;). For managed ecosystems, the main source of N is
fertilisation which is reflected in a peak value of &amp;chi;&lt;sub&gt;s&lt;/sub&gt; a few days following application, but also alters seasonal
values of NH&lt;sub&gt;4 apo&lt;/sub&gt;&lt;sup+&lt;/sup&gt; and NH&lt;sub&gt;4 bulk&lt;/sub&gt;&lt;sup+&lt;/sup&gt;. We propose a
parameterisation for &amp;chi;&lt;sub&gt;s&lt;/sub&gt; which includes peak values as a
function of amount and type of fertiliser application which gradually
decreases to a background value. The background &amp;chi;&lt;sub&gt;s&lt;/sub&gt; is
based on total N input to the ecosystem as a yearly fertiliser application
and N deposition (&lt;i&gt;N&lt;/i&gt;&lt;sub&gt;dep&lt;/sub&gt;). For non-managed ecosystems, &amp;chi;&lt;sub&gt;s&lt;/sub&gt; is parameterised based solely on the link with &lt;i&gt;N&lt;/i&gt;&lt;sub&gt;dep&lt;/sub&gt;.
&lt;br&gt;&lt;br&gt;
For &lt;i&gt;R&lt;/i&gt;&lt;sub&gt;w&lt;/sub&gt; we propose a general parameterisation as a function of
atmospheric relative humidity (RH), incorporating a minimum value
(&lt;i&gt;R&lt;/i&gt;&lt;sub&gt;w(min)&lt;/sub&gt;), which depends on the ratio of atmospheric acid concentrations
(SO&lt;sub&gt;2&lt;/sub&gt;, HNO&lt;sub&gt;3&lt;/sub&gt; and HCl) to NH&lt;sub&gt;3&lt;/sub&gt; concentrations. The
parameterisations are based mainly on datasets from temperate locations in
northern Europe making them most suitable for up-scaling in these regions
(EMEP model for example). In principle, the parameterisations should be
applicable to other climates, though there is a need for more underpinning
data, with the uncertainties being especially large for tropical and
subtropical conditions.</p>
</abstract>
<counts><page-count count="28"/></counts>
</article-meta>
</front>
<body/>
<back>
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