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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-24-2227-2006</article-id>
<title-group>
<article-title>Dayside flow bursts and high-latitude reconnection when the IMF is strongly  northward</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hu</surname>
<given-names>H.</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>Yeoman</surname>
<given-names>T. K.</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>Lester</surname>
<given-names>M.</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>Liu</surname>
<given-names>R.</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>Yang</surname>
<given-names>H.</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>Grocott</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>Polar Research Institute of China, Shanghai, China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Physics and Astronomy, University of Leicester, Leicester, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>13</day>
<month>09</month>
<year>2006</year>
</pub-date>
<volume>24</volume>
<issue>8</issue>
<fpage>2227</fpage>
<lpage>2242</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2006 H. Hu et al.</copyright-statement>
<copyright-year>2006</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/24/2227/2006/angeo-24-2227-2006.pdf">The full text article is available as a PDF file from https://angeo.copernicus.org/articles/24/2227/2006/angeo-24-2227-2006.pdf</self-uri>
<abstract>
<p>The characteristics of dayside ionospheric convection are
studied using Northern Hemispheric SuperDARN data and DMSP particle and flow
observations when the interplanetary magnetic field (IMF) was strongly
northward during 13:00&amp;ndash;15:00 UT on 2 March 2002. Although IMF &lt;i&gt;B&lt;sub&gt;x&lt;/sub&gt;&lt;/i&gt; was
positive, which is believed to favour Southern Hemisphere high-latitude
reconnection at equinox, a four-cell convection pattern was observed and
lasted for more than 1.5 h in the Northern Hemisphere. The reconnection
rate derived from an analysis of the Northern Hemisphere SuperDARN data
illustrates that the high-latitude reconnection was quasi-periodic, with a
period between 4&amp;ndash;16 min. A sawtooth-like and reverse-dispersed ion signature
was observed by DMSP-F14 in the sunward cusp convection at around 14:41 UT,
confirming that the high-latitude reconnection was pulsed. Accompanying the
pulsed reconnection, strong antisunward ionospheric flow bursts were
observed in the post-noon LLBL region on closed field lines, propagating with
the same speed as the plasma convection. DMSP flow data show that a similar
flow pattern and particle precipitation occurred in the conjugate Southern Hemisphere.</p>
</abstract>
<counts><page-count count="16"/></counts>
</article-meta>
</front>
<body/>
<back>
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