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<article language="en">
	<journal>
		<journal_title>Natural Hazards and Earth System Science</journal_title>
		<journal_url>www.nat-hazards-earth-syst-sci.net</journal_url>
		<issn>1561-8633</issn>
		<eissn>1684-9981</eissn>
		<volume_number>9</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/nhess-9-53-2009</doi>
	<article_url>http://www.nat-hazards-earth-syst-sci.net/9/53/2009/</article_url>
	<abstract_html>http://www.nat-hazards-earth-syst-sci.net/9/53/2009/nhess-9-53-2009.html</abstract_html>
	<fulltext_pdf>http://www.nat-hazards-earth-syst-sci.net/9/53/2009/nhess-9-53-2009.pdf</fulltext_pdf>
	<start_page>53</start_page>
	<end_page>59</end_page>
	<publication_date>2009-01-19</publication_date>
	<article_title content_type="html">Day-time variations of foF2 connected to strong earthquakes</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>E. V. Liperovskaya</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>V. V. Bogdanov</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>P.-F. Biagi</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>C.-V. Meister</name>
			<email>c.v.meister@skmail.ikp.physik.tu-darmstadt.de</email>
		</author>
		<author numeration="5" affiliations="1">
			<name>V. A. Liperovsky</name>
		</author>
		<author numeration="6" affiliations="5">
			<name>M. V. Rodkin</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Physics of the Earth of the Russian Academy of Sciences, Bolshaya Gruzinskaya 10, 123995 Moscow, Russia</affiliation>
		<affiliation numeration="2" content_type="html">Institute of Cosmophysical Research and Radio Wave Propagation, Far Eastern Branch of the Russian Academy of Sciences, 684034 Petropavlovsk-Kamchatsky, Russia</affiliation>
		<affiliation numeration="3" content_type="html">Physics Department, University of Bari, 70126 Bari, Italy</affiliation>
		<affiliation numeration="4" content_type="html">Technische Universität Darmstadt, Institut für Kernphysik, Schlossgartenstr. 9, 64289 Darmstadt, Germany</affiliation>
		<affiliation numeration="5" content_type="html">Geophysical Centre of the Russian Academy of Sciences, Molodejnaya 3, 117296 Moscow, Russia</affiliation>
	</affiliations>
	<abstract content_type="html">The statistical analysis of the characteristic frequency foF2 of the Earth&apos;s
ionosphere averaged over mid-day hours – from 11:00 till 17:00 h LT – is
carried out. Disturbances of foF2 connected to earthquakes are considered on
the background of seasonal, geomagnetic, 11-years and 27-days solar
variations. A special normalized parameter &lt;i&gt;F&lt;/i&gt; is introduced, which
represents the almost seasonal-independent part of foF2. Days with high solar
(Wolf number &gt;100) and geomagnetic (&amp;sum;&lt;i&gt;K&lt;sub&gt;p&lt;/sub&gt;&lt;/i&gt;&gt;30) activity are
excluded from the analysis. Events with magnitude &lt;i&gt;M&lt;/i&gt;&gt;5, distance from
the sounding station &lt;i&gt;R&lt;/i&gt;&lt;500 km and depth &lt;i&gt;h&lt;/i&gt;&lt;70 km are taken into
account. The superimposed epoches&apos; method is used to determine the temporal
dependence of &lt;i&gt;F&lt;/i&gt;. It is found that &lt;i&gt;F&lt;/i&gt;  increases about 3–6 days before
the earthquakes and then decreases one day – two days before the shock. The
decreased values of &lt;i&gt;F&lt;/i&gt;  continue to exist two-three days after events with
&lt;i&gt;M&lt;/i&gt;&gt;5.5. The obtained phenomenon depends on the magnitude of the
earthquake. For events with &lt;i&gt;M&lt;/i&gt;&gt;5.5, the reliability of the effect is
larger than 95%. For data of more than 80 earthquakes in the vicinity of
Petropavlovsk-Kamchatsky and more than 200 earthquakes in the vicinity of
Tokyo analogous results are obtained.</abstract>
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</article>

