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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>Springer Verlag</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.1007/s00585-999-0674-4</article-id>
<title-group>
<article-title>A slow mode wave as a possible source of Pi 2 and associated particle precipitation: a case study</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Saka</surname>
<given-names>O.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Watanabe</surname>
<given-names>O.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Okada</surname>
<given-names>K.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Baker</surname>
<given-names>D. N.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Physics, Kurume National College of Technology, Kurume , Japan</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>E-mail: saka@ges.kurume-nct.ac.jp</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Earth and Planetary Sciences, Kyushu University, Fukuoka, Japan</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>31</day>
<month>05</month>
<year>1999</year>
</pub-date>
<volume>17</volume>
<issue>5</issue>
<fpage>674</fpage>
<lpage>681</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 1999 O. Saka et al.</copyright-statement>
<copyright-year>1999</copyright-year>
<license license-type="open-access">
<license-p>© European Geosciences Union 1999</license-p>
</license>
</permissions>
<self-uri xlink:href="https://angeo.copernicus.org/articles/17/674/1999/angeo-17-674-1999.html">This article is available from https://angeo.copernicus.org/articles/17/674/1999/angeo-17-674-1999.html</self-uri>
<self-uri xlink:href="https://angeo.copernicus.org/articles/17/674/1999/angeo-17-674-1999.pdf">The full text article is available as a PDF file from https://angeo.copernicus.org/articles/17/674/1999/angeo-17-674-1999.pdf</self-uri>
<abstract>
<p>An intensification of auroral luminosity
referred to as an auroral break-up often accompanies the onset of geomagnetic
pulsation (Pi 2) at the dip-equator. One such auroral break-up occurred at 2239
UT on 16 June, 1986, being accompanied by weak substorm activity (AE~50 nT)
which was recorded in all-sky image of Syowa Station, Antarctica (66.2°S, 71.8°E
in geomagnetic coordinates). The associated Pi 2 magnetic pulsation was detected
by a fluxgate magnetometer in the afternoon sector at the dip-equator (Huancayo,
Peru; 1.44°N, 355.9° in geomagnetic coordinates; 12.1°S, 75.2°W in
geographic coordinates; &lt;i&gt;L&lt;/i&gt;=1.00). In spite of the large separation of the
two stations in longitude and latitude, the auroral break-up and subsequent
luminosity modulation were seen to be correlated with the wave form of the
ground Pi 2 pulsation. This occurred in such a way that the luminosity maximum
was seen to occur at the phase of maximum amplitudes of Pi 2 wave form. We argue
that the observed correlation could be interpreted as indicating a Pi
2-modulation of a field-aligned acceleration of the low energy electrons that
may occur near the equator of the midnight magnetosphere.&lt;br&gt;&lt;br&gt;&lt;b&gt;Key words.&lt;/b&gt; Magnetospheric physics (auroral phenomena;
energetic particles · precipitating; MHD waves and instabilities)</p>
</abstract>
<counts><page-count count="8"/></counts>
</article-meta>
</front>
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