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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ANGEO</journal-id>
<journal-title-group>
<journal-title>Annales Geophysicae</journal-title>
<abbrev-journal-title abbrev-type="publisher">ANGEO</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Ann. Geophys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1432-0576</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/angeo-22-935-2004</article-id>
<title-group>
<article-title>Influence of the Hall term on KH instability and reconnection inside KH vortices</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Nykyri</surname>
<given-names>K.</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>Otto</surname>
<given-names>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>The Blackett Laboratory, Imperial College, London, UK</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Geophysical Institute, University of Alaska, Fairbanks, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>19</day>
<month>03</month>
<year>2004</year>
</pub-date>
<volume>22</volume>
<issue>3</issue>
<fpage>935</fpage>
<lpage>949</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2004 K. Nykyri</copyright-statement>
<copyright-year>2004</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>
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<self-uri xlink:href="https://angeo.copernicus.org/articles/22/935/2004/angeo-22-935-2004.pdf">The full text article is available as a PDF file from https://angeo.copernicus.org/articles/22/935/2004/angeo-22-935-2004.pdf</self-uri>
<abstract>
<p>The Kelvin-Helmholtz instability (KHI) in its nonlinear stage can develop
  small-scale filamentary field and current structures at the flank
  boundaries of the magnetosphere. It has been shown previously with MHD
  simulations that magnetic reconnection can occur inside these narrow
  current layers, resulting in plasma transport from the solar wind into the
  magnetosphere. During periods of northward IMF, this transport is sufficient to generate a cold, dense plasma sheet on
  time scales consistent with satellite observations.
  However, when the
  length scales of these narrow current layers approach the ion inertia
  scale, the MHD approximation is not valid anymore and the Hall term in the
  Ohm&apos;s law must be included.  We will study the influence of the Hall term
  on the KHI with 2-D Hall-MHD simulations and compare our results with
  corresponding MHD simulations. We estimate plasma transport velocities of
  the order of ~1.5km/s, thus confirming the results of the MHD
  approximation.  However, the fine structure and the growth rates differ
  from the MHD approximation in an interesting way.&lt;br&gt;&lt;br&gt;
&lt;b&gt;Key words.&lt;/b&gt; Magnetospheric physics (magnetopause, cusp
and boundary layers; plasma waves and instabilities), Space
plasma physics (transport processes; magnetic reconnection;
numerical simulation studies; nonlinear phenomena; turbulence)</p>
</abstract>
<counts><page-count count="15"/></counts>
</article-meta>
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