Anomalies of LF signal during seismic activity in November–December 2004

A signal transmitted by Japan Time Standard LF station (40 kHz, Fukushima prefecture) and recorded in Petropavlovsk-Kamchatski (Russia) is analyzed during a time interval from 1 July 2004 till 24 January 2005. This interval is characterized by quiet seismic conditions up to the beginning o...

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Main Authors: A. A. Rozhnoi, M. S. Solovieva, O. A. Molchanov, M. Hayakawa, S. Maekawa, P. F. Biagi
Format: Article
Language:English
Published: Copernicus Publications 2005-01-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/5/657/2005/nhess-5-657-2005.pdf
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spelling doaj-fff942830f944a988eca45341b6ae0502020-11-24T23:09:01ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812005-01-0155657660Anomalies of LF signal during seismic activity in November–December 2004A. A. RozhnoiM. S. SolovievaO. A. MolchanovM. HayakawaS. MaekawaP. F. BiagiA signal transmitted by Japan Time Standard LF station (40 kHz, Fukushima prefecture) and recorded in Petropavlovsk-Kamchatski (Russia) is analyzed during a time interval from 1 July 2004 till 24 January 2005. This interval is characterized by quiet seismic conditions up to the beginning of November, but rather strong seismic activity occurs in November and December not far from Hokkaido (Japan) and in the region of northern Kuril Islands. There were three series of earthquakes with M=5.6–7.1 in a zone of sensitivity of our wave path during two months. Nighttime 'bay-like' phase and amplitude anomalies of the LF signal are observed several days before and during every series of earthquakes. During the whole period of seismic activity a significant shift in terminator times is also evident. The spectrum of LF seismo-induced anomalies shows a clear increase for the period of about 25 min.http://www.nat-hazards-earth-syst-sci.net/5/657/2005/nhess-5-657-2005.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. A. Rozhnoi
M. S. Solovieva
O. A. Molchanov
M. Hayakawa
S. Maekawa
P. F. Biagi
spellingShingle A. A. Rozhnoi
M. S. Solovieva
O. A. Molchanov
M. Hayakawa
S. Maekawa
P. F. Biagi
Anomalies of LF signal during seismic activity in November–December 2004
Natural Hazards and Earth System Sciences
author_facet A. A. Rozhnoi
M. S. Solovieva
O. A. Molchanov
M. Hayakawa
S. Maekawa
P. F. Biagi
author_sort A. A. Rozhnoi
title Anomalies of LF signal during seismic activity in November–December 2004
title_short Anomalies of LF signal during seismic activity in November–December 2004
title_full Anomalies of LF signal during seismic activity in November–December 2004
title_fullStr Anomalies of LF signal during seismic activity in November–December 2004
title_full_unstemmed Anomalies of LF signal during seismic activity in November–December 2004
title_sort anomalies of lf signal during seismic activity in november–december 2004
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2005-01-01
description A signal transmitted by Japan Time Standard LF station (40 kHz, Fukushima prefecture) and recorded in Petropavlovsk-Kamchatski (Russia) is analyzed during a time interval from 1 July 2004 till 24 January 2005. This interval is characterized by quiet seismic conditions up to the beginning of November, but rather strong seismic activity occurs in November and December not far from Hokkaido (Japan) and in the region of northern Kuril Islands. There were three series of earthquakes with M=5.6–7.1 in a zone of sensitivity of our wave path during two months. Nighttime 'bay-like' phase and amplitude anomalies of the LF signal are observed several days before and during every series of earthquakes. During the whole period of seismic activity a significant shift in terminator times is also evident. The spectrum of LF seismo-induced anomalies shows a clear increase for the period of about 25 min.
url http://www.nat-hazards-earth-syst-sci.net/5/657/2005/nhess-5-657-2005.pdf
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