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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ESDD</journal-id>
<journal-title-group>
<journal-title>Earth System Dynamics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ESDD</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Earth Syst. Dynam. Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">2190-4995</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/esdd-3-235-2012</article-id>
<title-group>
<article-title>Mathematical modelling of positive carbon-climate feedback: permafrost lake methane emission case</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sudakov</surname>
<given-names>I. 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>Vakulenko</surname>
<given-names>S. A.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>St. Petersburg State University of Technology and Design, Mathematics and Informatics Department, St. Petersburg, Russia</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute for Mechanical Engineering Problems, Russian Academy of Sciences, St. Petersburg, Russia</addr-line>
</aff>
<pub-date pub-type="epub">
<day>04</day>
<month>04</month>
<year>2012</year>
</pub-date>
<volume>3</volume>
<issue>1</issue>
<fpage>235</fpage>
<lpage>257</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2012 I. A. Sudakov</copyright-statement>
<copyright-year>2012</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://esd.copernicus.org/preprints/3/235/2012/esdd-3-235-2012.html">This article is available from https://esd.copernicus.org/preprints/3/235/2012/esdd-3-235-2012.html</self-uri>
<self-uri xlink:href="https://esd.copernicus.org/preprints/3/235/2012/esdd-3-235-2012.pdf">The full text article is available as a PDF file from https://esd.copernicus.org/preprints/3/235/2012/esdd-3-235-2012.pdf</self-uri>
<abstract>
<p>The permafrost methane emission problem is in the focus of attention of
different climate models. We present new approach to the permafrost methane
emission modeling. The tundra permafrost lakes is potential source of methane
emission. Typically, tundra landscape contains a number of small lakes and
warming leads to lake extension. We are making use of this process by the
nonlinear theory of phase transitions. We find that climate catastrophe
possibility depends on a feedback coefficient connecting the methane
concentration in atmosphere and temperature, and on the tundra permafrost
methane pool.</p>
</abstract>
<counts><page-count count="23"/></counts>
</article-meta>
</front>
<body/>
<back>
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