Preseismic ULF electromagnetic effect from observation at Kamchatka

Some results of ULF magnetic field observation at Karimshino site (Kamchatka, Russia) since June 2000 to September 2001 are presented here. Using case study we have found an effect of suppression of ULF intensity about 2–6 days before rather strong and nearby seismic shocks (magnitude M = 4.0 – 6.2)...

Full description

Bibliographic Details
Main Authors: O. Molchanov, A. Schekotov, E. Fedorov, G. Belyaev, E. Gordeev
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2003
Subjects:
G
Online Access:https://doaj.org/article/96ea222fedb74af69fff44020d025e54
id ftdoajarticles:oai:doaj.org/article:96ea222fedb74af69fff44020d025e54
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:96ea222fedb74af69fff44020d025e54 2023-05-15T16:58:49+02:00 Preseismic ULF electromagnetic effect from observation at Kamchatka O. Molchanov A. Schekotov E. Fedorov G. Belyaev E. Gordeev 2003-01-01T00:00:00Z https://doaj.org/article/96ea222fedb74af69fff44020d025e54 EN eng Copernicus Publications http://www.nat-hazards-earth-syst-sci.net/3/203/2003/nhess-3-203-2003.pdf https://doaj.org/toc/1561-8633 https://doaj.org/toc/1684-9981 1561-8633 1684-9981 https://doaj.org/article/96ea222fedb74af69fff44020d025e54 Natural Hazards and Earth System Sciences, Vol 3, Iss 3/4, Pp 203-209 (2003) Environmental technology. Sanitary engineering TD1-1066 Geography. Anthropology. Recreation G Environmental sciences GE1-350 Geology QE1-996.5 article 2003 ftdoajarticles 2022-12-31T14:07:39Z Some results of ULF magnetic field observation at Karimshino site (Kamchatka, Russia) since June 2000 to September 2001 are presented here. Using case study we have found an effect of suppression of ULF intensity about 2–6 days before rather strong and nearby seismic shocks (magnitude M = 4.0 – 6.2). It is revealed for nighttime and horizontal component of ULF field ( G ) in the frequency range 0.01 – 0.1 Hz. Then we prove the reliability of the effect by computed correlation between G (or 1/ G ) and specially calculated seismic indexes K s for the whole period of observation. Basing on the simple criteria we conclude that reliability of seismo-associated ULF suppression effect is comparable with well-known effect of connection between ULF variation and K p index of global magnetic activity. It seems the reason of suppression is located at the atmosphere or ionosphere but not in the ground medium. Article in Journal/Newspaper Kamchatka Directory of Open Access Journals: DOAJ Articles
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental technology. Sanitary engineering
TD1-1066
Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental technology. Sanitary engineering
TD1-1066
Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
Geology
QE1-996.5
O. Molchanov
A. Schekotov
E. Fedorov
G. Belyaev
E. Gordeev
Preseismic ULF electromagnetic effect from observation at Kamchatka
topic_facet Environmental technology. Sanitary engineering
TD1-1066
Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
Geology
QE1-996.5
description Some results of ULF magnetic field observation at Karimshino site (Kamchatka, Russia) since June 2000 to September 2001 are presented here. Using case study we have found an effect of suppression of ULF intensity about 2–6 days before rather strong and nearby seismic shocks (magnitude M = 4.0 – 6.2). It is revealed for nighttime and horizontal component of ULF field ( G ) in the frequency range 0.01 – 0.1 Hz. Then we prove the reliability of the effect by computed correlation between G (or 1/ G ) and specially calculated seismic indexes K s for the whole period of observation. Basing on the simple criteria we conclude that reliability of seismo-associated ULF suppression effect is comparable with well-known effect of connection between ULF variation and K p index of global magnetic activity. It seems the reason of suppression is located at the atmosphere or ionosphere but not in the ground medium.
format Article in Journal/Newspaper
author O. Molchanov
A. Schekotov
E. Fedorov
G. Belyaev
E. Gordeev
author_facet O. Molchanov
A. Schekotov
E. Fedorov
G. Belyaev
E. Gordeev
author_sort O. Molchanov
title Preseismic ULF electromagnetic effect from observation at Kamchatka
title_short Preseismic ULF electromagnetic effect from observation at Kamchatka
title_full Preseismic ULF electromagnetic effect from observation at Kamchatka
title_fullStr Preseismic ULF electromagnetic effect from observation at Kamchatka
title_full_unstemmed Preseismic ULF electromagnetic effect from observation at Kamchatka
title_sort preseismic ulf electromagnetic effect from observation at kamchatka
publisher Copernicus Publications
publishDate 2003
url https://doaj.org/article/96ea222fedb74af69fff44020d025e54
genre Kamchatka
genre_facet Kamchatka
op_source Natural Hazards and Earth System Sciences, Vol 3, Iss 3/4, Pp 203-209 (2003)
op_relation http://www.nat-hazards-earth-syst-sci.net/3/203/2003/nhess-3-203-2003.pdf
https://doaj.org/toc/1561-8633
https://doaj.org/toc/1684-9981
1561-8633
1684-9981
https://doaj.org/article/96ea222fedb74af69fff44020d025e54
_version_ 1766050929179623424