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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-26-3375-2008</article-id>
<title-group>
<article-title>Observations of vortex-like structure in the cusp-magnetosheath region during northward IMF orientation</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Tkachenko</surname>
<given-names>O.</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>Šafránková</surname>
<given-names>J.</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>Němeček</surname>
<given-names>Z.</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>Šimůnek</surname>
<given-names>J.</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>Přech</surname>
<given-names>L.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Charles University, Faculty of Mathematics and Physics, V Holesovickach 2, 180 00 Praha 8, Czech Republic</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute of Atmospheric Physics, Czech Academy of Science, Boční 1405, Praha 4, Czech Republic</addr-line>
</aff>
<pub-date pub-type="epub">
<day>22</day>
<month>10</month>
<year>2008</year>
</pub-date>
<volume>26</volume>
<issue>11</issue>
<fpage>3375</fpage>
<lpage>3387</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2008 O. Tkachenko et al.</copyright-statement>
<copyright-year>2008</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://angeo.copernicus.org/articles/26/3375/2008/angeo-26-3375-2008.html">This article is available from https://angeo.copernicus.org/articles/26/3375/2008/angeo-26-3375-2008.html</self-uri>
<self-uri xlink:href="https://angeo.copernicus.org/articles/26/3375/2008/angeo-26-3375-2008.pdf">The full text article is available as a PDF file from https://angeo.copernicus.org/articles/26/3375/2008/angeo-26-3375-2008.pdf</self-uri>
<abstract>
<p>Two-point observations made by the Interball spacecraft pair unveiled a presence of
a large vortex-like structure filled by slow and heated plasma in the outer
cusp during periods of the positive &lt;I&gt;B&lt;sub&gt;Z&lt;/sub&gt;&lt;/I&gt; interplanetary magnetic field (IMF)
component. We have observed the rotation of the magnetic field and the decrease
of its magnitude connected with the presence of a hot plasma population inside
the vortex. The structure starts with a clear reversal of the plasma
flow caused by reconnection tailward of the cusp that turns a part of the magnetosheath
plasma into the cusp. We compare the observations of two spacecraft in detail, discuss
the differences between them and suggest the way of a formation such structure.
Moreover, the statistical results have confirmed that this phenomenon is probably a regular feature
of the high-altitude cusp, however, this relatively small structure cannot be
observed too often. The alternative explanation of presented observations as a
flapping of the magnetopause is taken into account and discussed.</p>
</abstract>
<counts><page-count count="13"/></counts>
</article-meta>
</front>
<body/>
<back>
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