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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-13-7183-2013</article-id>
<title-group>
<article-title>Simulations of the transport and deposition of &lt;sup&gt;137&lt;/sup&gt;Cs over Europe after the Chernobyl Nuclear Power Plant accident: influence of varying emission-altitude and model horizontal and vertical resolution</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Evangeliou</surname>
<given-names>N.</given-names>
<ext-link>https://orcid.org/0000-0001-7196-1018</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Balkanski</surname>
<given-names>Y.</given-names>
<ext-link>https://orcid.org/0000-0001-8241-2858</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Cozic</surname>
<given-names>A.</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>Møller</surname>
<given-names>A. P.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Laboratoire des Sciences du Climat et de l&apos;Environnement (LSCE), CEA-UVSQ-CNRS UMR8212, Institut Pierre et Simon Laplace, L&apos;Orme des Merisiers, 91191 Gif sur Yvette Cedex, France</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Laboratoire d&apos;Ecologie, Systématique et Evolution, CNRS UMR8079, Université Paris-Sud, Bâtiment 362, 91405 Orsay Cedex, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>29</day>
<month>07</month>
<year>2013</year>
</pub-date>
<volume>13</volume>
<issue>14</issue>
<fpage>7183</fpage>
<lpage>7198</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 N. Evangeliou et al.</copyright-statement>
<copyright-year>2013</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/13/7183/2013/acp-13-7183-2013.html">This article is available from https://acp.copernicus.org/articles/13/7183/2013/acp-13-7183-2013.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/13/7183/2013/acp-13-7183-2013.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/13/7183/2013/acp-13-7183-2013.pdf</self-uri>
<abstract>
<p>The coupled model LMDZORINCA has been used to simulate the transport, wet
and dry deposition of the radioactive tracer &lt;sup&gt;137&lt;/sup&gt;Cs after accidental
releases. For that reason, two horizontal resolutions were deployed and used
in the model, a regular grid of 2.5° × 1.27°, and the same
grid stretched over Europe to reach a resolution of 0.66° × 0.51°. The vertical dimension is represented with two different
resolutions, 19 and 39 levels respectively, extending up to the mesopause. Four
different simulations are presented in this work; the first uses the regular
grid over 19 vertical levels assuming that the emissions took place at the
surface (RG19L(S)), the second also uses the regular grid over 19 vertical
levels but realistic source injection heights (RG19L); in the third
resolution the grid is regular and the vertical resolution 39 levels (RG39L)
and finally, it is extended to the stretched grid with 19 vertical levels
(Z19L). The model is validated with the Chernobyl accident which occurred in
Ukraine (ex-USSR) on 26 May 1986 using the emission inventory from
Brandt et al. (2002). This accident has been widely studied since 1986, and
a large database has been created containing measurements of atmospheric
activity concentration and total cumulative deposition for &lt;sup&gt;137&lt;/sup&gt;Cs from
most of the European countries.
&lt;br&gt;&lt;br&gt;
According to the results, the performance of the model to predict the
transport and deposition of the radioactive tracer was efficient and
accurate presenting low biases in activity concentrations and deposition
inventories, despite the large uncertainties on the intensity of the source
released. The best agreement with observations was obtained using the
highest horizontal resolution of the model (Z19L run). The model managed to
predict the radioactive contamination in most of the European regions
(similar to De Cort et al., 1998), and also the arrival times of the
radioactive fallout. As regards to the vertical resolution, the largest
biases were obtained for the 39 layers run due to the increase of the levels
in conjunction with the uncertainty of the source term. Moreover, the
ecological half-life of &lt;sup&gt;137&lt;/sup&gt;Cs in the atmosphere after the accident
ranged between 6 and 9 days, which is in good accordance to what previously
reported and in the same range with the recent accident in Japan. The high
response of LMDZORINCA model for &lt;sup&gt;137&lt;/sup&gt;Cs reinforces the importance of
atmospheric modelling in emergency cases to gather information for protecting
the population from the adverse effects of radiation.</p>
</abstract>
<counts><page-count count="16"/></counts>
</article-meta>
</front>
<body/>
<back>
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