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<front>
<journal-meta>
<journal-id journal-id-type="publisher">NPG</journal-id>
<journal-title-group>
<journal-title>Nonlinear Processes in Geophysics</journal-title>
<abbrev-journal-title abbrev-type="publisher">NPG</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Nonlin. Processes Geophys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1607-7946</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/npg-20-543-2013</article-id>
<title-group>
<article-title>Stability and nonlinear regimes of flow over a saturated porous medium</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lyubimova</surname>
<given-names>T. P.</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>Baydina</surname>
<given-names>D. T.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lyubimov</surname>
<given-names>D. V.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute of Continuous Media Mechanics, Ural Branch of RAS, Perm,  Russia</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Perm State University, Theoretical Physics Department,  Perm, Russia</addr-line>
</aff>
<pub-date pub-type="epub">
<day>23</day>
<month>07</month>
<year>2013</year>
</pub-date>
<volume>20</volume>
<issue>4</issue>
<fpage>543</fpage>
<lpage>547</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 T. P. Lyubimova 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://npg.copernicus.org/articles/20/543/2013/npg-20-543-2013.html">This article is available from https://npg.copernicus.org/articles/20/543/2013/npg-20-543-2013.html</self-uri>
<self-uri xlink:href="https://npg.copernicus.org/articles/20/543/2013/npg-20-543-2013.pdf">The full text article is available as a PDF file from https://npg.copernicus.org/articles/20/543/2013/npg-20-543-2013.pdf</self-uri>
<abstract>
<p>The paper deals with the investigation of stability and nonlinear regimes of
flow over the saturated porous medium applied to the problem of stability of
water flow over the bottom covered with vegetation. It is shown that the
velocity profile of steady plane-parallel flow has two inflection points,
which results in instability of this flow. The neutral stability curves, the
dependencies of critical Reynolds number and the wave number of most
dangerous perturbations on the ratio of porous layer thickness to the total
thickness are obtained. The nonlinear flow regimes are investigated
numerically by finite difference method. It is found that at supercritical
parameter values waves travelling in the direction of the base flow take
place.</p>
</abstract>
<counts><page-count count="5"/></counts>
</article-meta>
</front>
<body/>
<back>
<ref-list>
<title>References</title>
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</back>
</article>