<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.nat-hazards-earth-syst-sci.net/inc/nhess/copernicus.dtd">
<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>8</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/nhess-8-129-2008</doi>
	<article_url>http://www.nat-hazards-earth-syst-sci.net/8/129/2008/</article_url>
	<abstract_html>http://www.nat-hazards-earth-syst-sci.net/8/129/2008/nhess-8-129-2008.html</abstract_html>
	<fulltext_pdf>http://www.nat-hazards-earth-syst-sci.net/8/129/2008/nhess-8-129-2008.pdf</fulltext_pdf>
	<start_page>129</start_page>
	<end_page>134</end_page>
	<publication_date>2008-02-25</publication_date>
	<article_title content_type="html">On the generation mechanism of terminator times in subionospheric VLF/LF propagation and its possible application to seismogenic effects</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. Yoshida</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>T. Yamauchi</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>T. Horie</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>M. Hayakawa</name>
			<email>hayakawa@whistler.ee.uec.ac.jp</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Electronic Engineering and Research Station on Seismo Electromagnetics, University of Electro-Communications, 1-5-1 Chofugaoka, Chofu Tokyo 182-8585, Japan</affiliation>
	</affiliations>
	<abstract content_type="html">The signals from VLF/LF transmitters are known to propagate in the
Earth-ionosphere waveguide, so that the subionospheric propagation
characteristics are very sensitive to the condition of the lower ionosphere.
We know that there appear the terminator times just around the sunrise and
sunset in the diurnal variation of subionospheric VLF/LF signal (amplitude
and phase). These terminator times are found to shift significantly just
around an earthquake, which enables us to infer the change in the ionosphere
during the earthquake. In this paper we try to understand the physical
mechanism on the generation of those terminator times for relatively short
propagation path (less than 2000 km) by means of wave-hop method. It is
found that the lowering of the ionosphere boundary during an earthquake
decreases the path length of the sky wave and this alters the interference
condition of this wave with the ground wave, which lead to an appearance of
terminator times as the destructive interference between the ground and sky
waves. Finally, we suggest a possible use of terminator time shifts to
investigate the lower ionospheric plasma changes during the earthquakes.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Belrose, J. S.: Low and very low frequency radio wave propagation, in Radio Wave Propagation, AGARD Lecture Ser., 29, 97&amp;ndash;115, Advisory Group for Aerospace Research and Development, NATO, France, 1968. </reference>
		<reference numeration="2" content_type="text"> Biagi, P. F., Castella, L., Maggipinto, T., Ermini, A., Perna, G., and Capozzi, V.: Electric field strength analysis of 216 and 270 kHz broadcast signals recorded during 9 years, Radio Sci., 41, RS4013, doi:10.1029/2005RS003296, 2006. </reference>
		<reference numeration="3" content_type="text"> Budden, K. G.: The Wave-Guide Mode Theory of Wave Propagation, Logos Press, London, 325 pp., 1961. </reference>
		<reference numeration="4" content_type="text"> Hayakawa, M. and Molchanov, O. A.: Seismo Electromagnetics: Lithosphere &amp;ndash; Atmosphere &amp;ndash; Ionosphere Coupling, TERRAPUB, Tokyo, 477 pp., 2002. </reference>
		<reference numeration="5" content_type="text"> Hayakawa, M. and Fujinawa, Y.: Electromagnetic Phenomena Related to Earthquake Prediction, Terra Sci. Pub. Co., Tokyo, 667 pp., 1994. </reference>
		<reference numeration="6" content_type="text"> Hayakawa, M., Molchanov, O. A., Ondoh, T., and Kawai, E.: The precursory signature effect of the Kobe earthquake on VLF subionospheric signals, J. Comm. Res. Lab., Tokyo, 43, 169&amp;ndash;180, 1996. </reference>
		<reference numeration="7" content_type="text"> Hayakawa, M.: Atmospheric and Ionospheric Electromagnetic Phenomena Associated with Earthquakes, Terra Sci. Pub. Co., Tokyo, 996 pp., 1999. </reference>
		<reference numeration="8" content_type="text"> Hayakawa, M. and Molchanov, O. A.: NASDA/UEC team, Summary report of NASDA&apos;s earthquake remote sensing frontier project, Phys. Chem. Earth, 29, 617&amp;ndash;625, 2004. </reference>
		<reference numeration="9" content_type="text"> International Telecommunication Union, Recommendation ITU-R, Ground wave propagation curves for frequencies between 10 kHz and 3 DMHz,Geneva, Switzerland, P. Series, p. 368&amp;ndash;7,1992. </reference>
		<reference numeration="10" content_type="text"> International Telecommunication Union, Recommendation ITU-R, Prediction of field strength at frequencies below 150 kHz, Geneva, Switzerland, P. Series, p. 684-3, 2002. </reference>
		<reference numeration="11" content_type="text"> Maekawa, S., Horie, T., Yamauchi, T., Sawaya, T., Ishikawa, M., Hayakawa, M., and Sasaki, H.: A statistical study on the effect of earthquakes on the ionosphere, based on the subionospheric LF propagation data in Japan, Ann. Geophys., 24, 2219&amp;ndash;2225, 2006. </reference>
		<reference numeration="12" content_type="text"> Molchanov, O. A. and Hayakawa, M.: Subionospheric VLF signal perturbations possibly related to earthquakes, J. Geophys. Res., 103, 17 489&amp;ndash;17 504, 1998. </reference>
		<reference numeration="13" content_type="text"> Molchanov, O. A., Hayakawa, M., Ondoh, T., and Kawai, E.: Precursory effects in the subionospheric VLF signals for the Kobe earthquake, Phys. Earth Planet. In., 105, 239&amp;ndash;248, 1998. </reference>
		<reference numeration="14" content_type="text"> Rozhnoi, A., Solovieva, M. S., Molchanov, O. A., and Hayakawa, M.: Middle latitude LF (40 kHz) phase variations associated with earthquakes for quiet and disturbed geomagnetic conditions, Phys. Chem. Earth, 29, 589&amp;ndash;598, 2004. </reference>
		<reference numeration="15" content_type="text"> Shvets, A. V., Hayakawa, M., Molchanov, O. A., and Ando, Y.: A study of ionospheric response to regional seismic activity by VLF radio sounding, Phys. Chem. Earth, 29, 627&amp;ndash;637, 2004. </reference>
		<reference numeration="16" content_type="text"> Wakai, N., Kurihara, N., Otsuka, A., and Imamura, K.: Prediction method of LF/MF field strangths, Inst. Electr. Information Comm. Engrs. Japan, Technical Report, AP-2003-271, 35&amp;ndash;40, 2004. </reference>
	</references>
</article>

