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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-22-63-2004</article-id>
<title-group>
<article-title>Evaluation of the geometry of ionospheric current systems related to rapid geomagnetic variations</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Apatenkov</surname>
<given-names>S. V.</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>Sergeev</surname>
<given-names>V. 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>Pirjola</surname>
<given-names>R.</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>Viljanen</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>Institute of Physics, St. Petersburg State University, Ulyanovskaya 1, Petrodvoretz, 198504, St.Petersburg, Russia</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Finnish Meteorological Institute, Geophysical Research Division, P.O. Box 503, FIN-00101 Helsinki, Finland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>01</day>
<month>01</month>
<year>2004</year>
</pub-date>
<volume>22</volume>
<issue>1</issue>
<fpage>63</fpage>
<lpage>72</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2004 S. V. Apatenkov et al.</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>
<self-uri xlink:href="https://angeo.copernicus.org/articles/22/63/2004/angeo-22-63-2004.html">This article is available from https://angeo.copernicus.org/articles/22/63/2004/angeo-22-63-2004.html</self-uri>
<self-uri xlink:href="https://angeo.copernicus.org/articles/22/63/2004/angeo-22-63-2004.pdf">The full text article is available as a PDF file from https://angeo.copernicus.org/articles/22/63/2004/angeo-22-63-2004.pdf</self-uri>
<abstract>
<p>To learn about the geometry and sources of the ionospheric current
systems which generate strong geomagnetically induced currents, we
categorize differential equivalent current systems (DEC) for
events with strong &lt;i&gt;dB/dt&lt;/i&gt; by decomposing them into the
contributions of electrojet-type and vortex-type elementary
systems. By solving the inverse problem we obtain amplitudes and
locations of these elementary current systems. One-minute
differences of the geomagnetic field values at the IMAGE
magnetometer network in 1996–2000 are analysed to study the
spatial distributions of large &lt;i&gt;dB/dt&lt;/i&gt; events. The relative
contributions of the two components are evaluated. In particular, we
found that the majority of the strongest &lt;i&gt;dB/dt&lt;/i&gt; events (100–1000nT/min) appear to be produced by the vortex-type current
structures and most of them occur in the morning LT hours, probably
caused by the Ps6 pulsation events associated with auroral omega
structures. For strong &lt;i&gt;dB/dt&lt;/i&gt; events the solar wind parameters are
shifted toward strong (tens nT) southward IMF, enhanced velocity
and dynamic pressure, in order for the main phase of
the magnetic storms to occur. Although these events appear mostly during
magnetic storms when the auroral oval greatly expands, the area of
large &lt;i&gt;dB/dt&lt;/i&gt; stays in the middle part of the auroral zone;
therefore, it is connected to the processes taking part in the
middle of the magnetosphere rather than in its innermost region
populated by the ring current.&lt;br&gt;&lt;br&gt;
&lt;b&gt;Key words.&lt;/b&gt;
Geomagnetism and paleomagnetism (rapid time variations) –
Ionosphere (auroral ionosphere; ionospheric disturbances)</p>
</abstract>
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