Low-Latitude Atmosphere-Ionosphere Effects Initiated by Strong Earthquakes Preparation Process

Ionospheric and atmospheric anomalies registered around the time of strong earthquakes in low-latitude regions are reported now regularly. Majority of these reports have the character of case studies without clear physical mechanism proposed. Here we try to present the general conception of low-lati...

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Main Author: Sergey Pulinets
Format: Article
Language:English
Published: Hindawi Limited 2012-01-01
Series:International Journal of Geophysics
Online Access:http://dx.doi.org/10.1155/2012/131842
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spelling doaj-6836552a62c84469bb759fb6211699722020-11-24T23:18:47ZengHindawi LimitedInternational Journal of Geophysics1687-885X1687-88682012-01-01201210.1155/2012/131842131842Low-Latitude Atmosphere-Ionosphere Effects Initiated by Strong Earthquakes Preparation ProcessSergey Pulinets0Space Research Institute, Russian Academy of Sciences, Moscow 117997, RussiaIonospheric and atmospheric anomalies registered around the time of strong earthquakes in low-latitude regions are reported now regularly. Majority of these reports have the character of case studies without clear physical mechanism proposed. Here we try to present the general conception of low-latitude effects using the results of the recent author’s publications, including also rethinking the earlier results interpreted basing on recently established background physical mechanisms of anomalies generation. It should be underlined that only processes initiated by earthquake preparation are considered. Segregation of low-latitude regions for special consideration is connected with the important role of ionospheric equatorial anomaly in the seismoionospheric coupling and specific character of low-latitude earthquake initiated effects. Three main specific features can be marked in low-latitude ionospheric anomalies manifestation: the presence of magnetic conjugacy in majority of cases, local longitudinal asymmetry of effects observed in ionosphere in relation to the vertical projection of epicenter onto ionosphere, and equatorial anomaly reaction even on earthquakes outside equatorial anomaly (i.e., 30–40 LAT). The equality of effects morphology regardless they observed over land or over sea implies only one possible explanation that these anomalies are initiated by gaseous emanations from the Earth crust, and radon plays the major role.http://dx.doi.org/10.1155/2012/131842
collection DOAJ
language English
format Article
sources DOAJ
author Sergey Pulinets
spellingShingle Sergey Pulinets
Low-Latitude Atmosphere-Ionosphere Effects Initiated by Strong Earthquakes Preparation Process
International Journal of Geophysics
author_facet Sergey Pulinets
author_sort Sergey Pulinets
title Low-Latitude Atmosphere-Ionosphere Effects Initiated by Strong Earthquakes Preparation Process
title_short Low-Latitude Atmosphere-Ionosphere Effects Initiated by Strong Earthquakes Preparation Process
title_full Low-Latitude Atmosphere-Ionosphere Effects Initiated by Strong Earthquakes Preparation Process
title_fullStr Low-Latitude Atmosphere-Ionosphere Effects Initiated by Strong Earthquakes Preparation Process
title_full_unstemmed Low-Latitude Atmosphere-Ionosphere Effects Initiated by Strong Earthquakes Preparation Process
title_sort low-latitude atmosphere-ionosphere effects initiated by strong earthquakes preparation process
publisher Hindawi Limited
series International Journal of Geophysics
issn 1687-885X
1687-8868
publishDate 2012-01-01
description Ionospheric and atmospheric anomalies registered around the time of strong earthquakes in low-latitude regions are reported now regularly. Majority of these reports have the character of case studies without clear physical mechanism proposed. Here we try to present the general conception of low-latitude effects using the results of the recent author’s publications, including also rethinking the earlier results interpreted basing on recently established background physical mechanisms of anomalies generation. It should be underlined that only processes initiated by earthquake preparation are considered. Segregation of low-latitude regions for special consideration is connected with the important role of ionospheric equatorial anomaly in the seismoionospheric coupling and specific character of low-latitude earthquake initiated effects. Three main specific features can be marked in low-latitude ionospheric anomalies manifestation: the presence of magnetic conjugacy in majority of cases, local longitudinal asymmetry of effects observed in ionosphere in relation to the vertical projection of epicenter onto ionosphere, and equatorial anomaly reaction even on earthquakes outside equatorial anomaly (i.e., 30–40 LAT). The equality of effects morphology regardless they observed over land or over sea implies only one possible explanation that these anomalies are initiated by gaseous emanations from the Earth crust, and radon plays the major role.
url http://dx.doi.org/10.1155/2012/131842
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