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<!DOCTYPE article SYSTEM "http://www.nonlin-processes-geophys.net/inc/npg/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Nonlinear Processes  in Geophysics</journal_title>
		<journal_url>www.nonlin-processes-geophys.net</journal_url>
		<issn>1023-5809</issn>
		<eissn>1607-7946</eissn>
		<volume_number>10</volume_number>
		<issue_number>1/2</issue_number>
		<publication_year>2003</publication_year>
	</journal>
	<doi>10.5194/npg-10-13-2003</doi>
	<article_url>http://www.nonlin-processes-geophys.net/10/13/2003/</article_url>
	<abstract_html>http://www.nonlin-processes-geophys.net/10/13/2003/npg-10-13-2003.html</abstract_html>
	<fulltext_pdf>http://www.nonlin-processes-geophys.net/10/13/2003/npg-10-13-2003.pdf</fulltext_pdf>
	<start_page>13</start_page>
	<end_page>26</end_page>
	<publication_date>0000-00-00</publication_date>
	<article_title content_type="html">Large amplitude solitary waves in and near the Earth’s magnetosphere, magnetopause and bow shock: Polar and Cluster observations</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>C. Cattell</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>C. Neiman</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>J. Dombeck</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>J. Crumley</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>J. Wygant</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>C. A. Kletzing</name>
		</author>
		<author numeration="7" affiliations="3">
			<name>W. K. Peterson</name>
		</author>
		<author numeration="8" affiliations="4">
			<name>F. S. Mozer</name>
		</author>
		<author numeration="9" affiliations="5">
			<name>M. André</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">School of Physics and Astronomy, University of Minnesota, Minneapolis, MN 55455, USA</affiliation>
		<affiliation numeration="2" content_type="html">Dept. of Physics and Astronomy, University of Iowa, Iowa City, IA 52242, USA</affiliation>
		<affiliation numeration="3" content_type="html">Lockheed Martin Space Sciences Laboratory, Palo Alto, CA 94304, USA</affiliation>
		<affiliation numeration="4" content_type="html">Space Sciences Laboratory, University of California, Berkeley, CA 94720, USA</affiliation>
		<affiliation numeration="5" content_type="html">Swedish Institute for Space Physics, Uppsala, Sweden</affiliation>
	</affiliations>
	<abstract content_type="html">Solitary waves with
      large electric fields (up to 100&apos;s of mV/m) have been observed
      throughout the magnetosphere and in the bow shock. We discuss observations
      by Polar at high altitudes ( ~ 4-8 RE ), during crossings of the plasma
      sheet boundary and cusp, and new measurements by Polar at the equatorial
      magnetopause and by Cluster near the bow shock, in the cusp and at the
      plasma sheet boundary. We describe the results of a statistical study of
      electron solitary waves observed by Polar at high altitudes. The mean
      solitary wave duration was ~ 2 ms. The waves have velocities from ~ 1000
      km/s to&amp;nbsp; &amp;gt; 2500 km/s. Observed scale sizes (parallel to the
      magnetic field) are on the order of 1-10&lt;font face=&quot;Symbol&quot;&gt;l&lt;/font&gt;&lt;sub&gt;D&lt;/sub&gt;,
      with &lt;i&gt;e&lt;font face=&quot;Symbol&quot;&gt;F&lt;/font&gt;/kT&lt;sub&gt;e&lt;/sub&gt;&lt;/i&gt; from ~ 0.01 to
      O(1). The average speed of solitary waves at the plasma sheet boundary is
      faster than the average speed observed in the cusp and at cusp injections.
      The amplitude increases with both velocity and scale size. These
      observations are all consistent with the identification of the solitary
      waves as electron hole modes. We also report the discovery of solitary
      waves at the magnetopause, observed in Polar data obtained at the subsolar
      equatorial magnetopause. Both positive and negative potential structures
      have been observed with amplitudes up to ~ 25 mV/m. The velocities range
      from 150 km/s to &amp;gt;2500 km/s, with scale sizes the order of a kilometer
      (comparable to the Debye length). Initial observations of solitary waves
      by the four Cluster satellites are utilized to discuss the scale sizes and
      time variability of the regions where the solitary waves occur.
      Preliminary results from the four Cluster satellites have given a glimpse
      of the spatial and temporal variability of the occurrence of solitary
      waves and their association with other wave modes. In all the events
      studied, significant differences were observed in the waveforms observed
      simultaneously at the four locations separated by ~ 1000 km. When solitary
      waves were seen at one satellite, they were usually also seen at the other
      satellites within an interval of a few seconds. In association with an
      energetic electron injection and a highly compressed magnetosphere,
      Cluster has observed the largest amplitude solitary waves (&amp;gt;750 mV/m)
      ever reported in the outer magnetosphere.</abstract>
	<references>
	</references>
</article>

