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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-3-747-2003</article-id>
<title-group>
<article-title>Methodology for prediction and estimation of consequences of possible atmospheric releases of hazardous matter: &quot;Kursk&quot; submarine study</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Baklanov</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>Mahura</surname>
<given-names>A.</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>Sørensen</surname>
<given-names>J. H.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Danish Meteorological Institute, 2100 Copenhagen, Denmark</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Kola Science Centre, Apatity, 184200, Russia</addr-line>
</aff>
<pub-date pub-type="epub">
<day>18</day>
<month>06</month>
<year>2003</year>
</pub-date>
<volume>3</volume>
<issue>3</issue>
<fpage>747</fpage>
<lpage>762</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2003 A. Baklanov et al.</copyright-statement>
<copyright-year>2003</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 Generic License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by-nc-sa/2.5/">https://creativecommons.org/licenses/by-nc-sa/2.5/</ext-link></license-p>
</license>
</permissions>
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<self-uri xlink:href="https://acp.copernicus.org/articles/3/747/2003/acp-3-747-2003.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/3/747/2003/acp-3-747-2003.pdf</self-uri>
<abstract>
<p>There are objects with some periods of higher than normal levels of risk of accidental atmospheric releases
      (nuclear, chemical, biological, etc.). Such accidents or events may occur due to natural hazards, human
      errors, terror acts, and during transportation of waste or various operations at high risk. A methodology for
      risk assessment is suggested and it includes two approaches: 1) probabilistic analysis of possible atmospheric
      transport patterns using long-term trajectory and dispersion modelling, and 2) forecast and evaluation of
      possible contamination and consequences for the environment and population using operational dispersion
      modelling. The first approach could be applied during the preparation stage, and the second
      - during the operation stage. The suggested methodology is applied on an example of the most important phases (lifting,
      transportation, and decommissioning) of the ``Kursk&amp;quot; nuclear submarine operation.&lt;br&gt;
      &lt;br&gt;
      It is found that the temporal variability of several probabilistic indicators (fast transport probability fields,
      maximum reaching distance, maximum possible impact zone, and average integral concentration of
      &lt;sup&gt;137&lt;/sup&gt;Cs) showed that the fall of 2001 was the most appropriate time for the beginning of the operation. These
      indicators allowed to identify the hypothetically impacted geographical regions and territories. In cases of
      atmospheric transport toward the most populated areas, the forecasts of possible consequences during phases
      of the high and medium potential risk levels based on a unit hypothetical release (e.g.
      1 Bq) are performed. The analysis showed that the possible deposition fractions of
      10&lt;sup&gt;-11&lt;/sup&gt; (Bq/m&lt;sup&gt;2&lt;/sup&gt;) over the Kola Peninsula, and 10&lt;sup&gt;-12
      &lt;/sup&gt;- 10&lt;sup&gt;-13&lt;/sup&gt; (Bq/m&lt;sup&gt;2&lt;/sup&gt;) for the remote areas of the Scandinavia and Northwest Russia could be observed.&lt;br&gt;
      &lt;br&gt;
      The suggested methodology may be used successfully for any potentially dangerous object involving risk of
      atmospheric release of hazardous materials of nuclear, chemical or biological nature.</p>
</abstract>
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