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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</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/acpd-6-13111-2006</article-id>
<title-group>
<article-title>Behaviour of tracer diffusion in simple atmospheric boundary layer models</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Anderson</surname>
<given-names>P. S.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>British Antarctic Survey, Madingley Road, Cambridge, CB3 0ET, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>13</day>
<month>12</month>
<year>2006</year>
</pub-date>
<volume>6</volume>
<issue>6</issue>
<fpage>13111</fpage>
<lpage>13138</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>
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<abstract>
<p>1-D profiles and time series from an idealised atmospheric boundary layer
model are presented, which show agreement with measurements of polar
photogenic NO and NO&lt;sub&gt;2&lt;/sub&gt;. Diffusion models are increasingly being used as
the framework for studying tropospheric air chemistry dynamics. Models based
on standard boundary layer diffusivity profiles have an intrinsic behaviour
that is not necessarily intuitive, due to the variation of turbulent
diffusivity with height. The relatively simple model provides both a
programming and a conceptual tool in the analysis of observed trace gas
evolution. A time scale inherent in the model can be tuned by fitting model
time series to observations. This scale is then applicable to the more
physically simple but chemically complex zeroth order or box models of
chemical interactions.</p>
</abstract>
<counts><page-count count="28"/></counts>
</article-meta>
</front>
<body/>
<back>
<ref-list>
<title>References</title>
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<label>5</label><mixed-citation publication-type="other" xlink:type="simple"> King, J. C. and Anderson, P. S.: Heat and Water Vapour fluxes and Scalar Roughness Lengths over an Antarctic Ice Shelf, Bound.-Layer Meteorol., 69, 101&amp;ndash;121, 1994. </mixed-citation>
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<label>6</label><mixed-citation publication-type="other" xlink:type="simple"> King, J. C., Argentini, S. A., and Anderson, P. S.: Contrasts between summer time surface energy balance and boundary layer structure at Dome C and Halley stations, Antarctica, J. Geophys. Res., 111, D02105, doi:10.1029/2005JD006130, 2006. </mixed-citation>
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</back>
</article>