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<front>
<journal-meta>
<journal-id journal-id-type="publisher">NHESS</journal-id>
<journal-title-group>
<journal-title>Natural Hazards and Earth System Sciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">NHESS</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Nat. Hazards Earth Syst. Sci.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1684-9981</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/nhess-10-7-2010</article-id>
<title-group>
<article-title>Electron and ion density variations before strong earthquakes (&lt;i&gt;M&lt;/i&gt;&gt;6.0) using DEMETER and GPS data</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Akhoondzadeh</surname>
<given-names>M.</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>Parrot</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>Saradjian</surname>
<given-names>M. R.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Remote Sensing Division, Surveying and Geomatics Engineering Department, School of Engineering, University of Tehran, Tehran, Iran</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Laboratoire de Physique et Chimie de l&apos;Environnement et de l&apos;Espace (LPC2E)/CNRS, UMR6115, Orléans, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>11</day>
<month>01</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>1</issue>
<fpage>7</fpage>
<lpage>18</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2010 M. Akhoondzadeh et al.</copyright-statement>
<copyright-year>2010</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://nhess.copernicus.org/articles/10/7/2010/nhess-10-7-2010.html">This article is available from https://nhess.copernicus.org/articles/10/7/2010/nhess-10-7-2010.html</self-uri>
<self-uri xlink:href="https://nhess.copernicus.org/articles/10/7/2010/nhess-10-7-2010.pdf">The full text article is available as a PDF file from https://nhess.copernicus.org/articles/10/7/2010/nhess-10-7-2010.pdf</self-uri>
<abstract>
<p>Using IAP (plasma analyzer) and ISL (Langmuir probe) experiments onboard
DEMETER (Detection of Electromagnetic Emissions Transmitted from Earthquake
Regions) satellite and GPS (Global Positioning System) measurements, we have
statistically analyzed the variations of the electron and ion densities to
search for disturbances in the vicinity of four large earthquakes prior to
events. The indices &lt;i&gt;D&lt;/i&gt;&lt;sub&gt;st&lt;/sub&gt; and &lt;i&gt;K&lt;/i&gt;&lt;sub&gt;p&lt;/sub&gt; were used to distinguish
pre-earthquake anomalies from the other anomalies related to the geomagnetic
activities. For each studied case, a very good agreement was found between
the different parameters estimated by DEMETER and GPS data in the detection
of pre-seismic anomalies. Our statistics results show that the anomalous
deviations prior to earthquakes have different sign from case to case, and
that their amplitude depends on the magnitude of the earthquake. It has also
been found that the electron density measured by the ISL experiment at night
detects anomalous variations significantly before the earthquakes. The
appearance of positive and negative anomalies in both of DEMETER and TEC
(Total Electron Content) data during 1 to 5 days before all studied
earthquakes during quiet geomagnetic conditions indicates that these
anomalous behaviors are highly regarded as seismo-ionospheric precursors.</p>
</abstract>
<counts><page-count count="12"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>