Anomalous TEC variations associated with the powerful Tohoku earthquake of 11 March 2011

On 11 March 2011 at 14:46:23 LT, the 4th largest earthquake ever recorded with a magnitude of 9.0 occurred near the northeast coast of Honshu in Japan (38.322<sup>°</sup> N, 142.369<sup>°</sup> E, Focal depth 29.0 km). I...

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Main Author: M. Akhoondzadeh
Format: Article
Language:English
Published: Copernicus Publications 2012-05-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/12/1453/2012/nhess-12-1453-2012.pdf
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spelling doaj-143ff2b803b84c03ae109aef5fcc7b4d2020-11-24T23:01:31ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812012-05-011251453146210.5194/nhess-12-1453-2012Anomalous TEC variations associated with the powerful Tohoku earthquake of 11 March 2011M. AkhoondzadehOn 11 March 2011 at 14:46:23 LT, the 4th largest earthquake ever recorded with a magnitude of 9.0 occurred near the northeast coast of Honshu in Japan (38.322<sup>°</sup> N, 142.369<sup>°</sup> E, Focal depth 29.0 km). In order to acknowledge the capabilities of Total Electron Content (TEC) ionospheric precursor, in this study four methods including mean, median, wavelet transform, and Kalman filter have been applied to detect anomalous TEC variations concerning the Tohoku earthquake. The duration of the TEC time series dataset is 49 days at a time resolution of 2 h. All four methods detected a considerable number of anomalous occurrences during 1 to 10 days prior to the earthquake in a period of high geomagnetic activities. In this study, geomagnetic indices (i.e. <i>D</i><sub>st</sub>, <i>K</i><sub><i>p</i></sub>, <i>A</i><sub><i>p</i></sub> and <i>F</i>10.7) were used to distinguish pre-earthquake anomalies from the other anomalies related to the geomagnetic and solar activities. A good agreement in results was found between the different applied anomaly detection methods on TEC data.http://www.nat-hazards-earth-syst-sci.net/12/1453/2012/nhess-12-1453-2012.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. Akhoondzadeh
spellingShingle M. Akhoondzadeh
Anomalous TEC variations associated with the powerful Tohoku earthquake of 11 March 2011
Natural Hazards and Earth System Sciences
author_facet M. Akhoondzadeh
author_sort M. Akhoondzadeh
title Anomalous TEC variations associated with the powerful Tohoku earthquake of 11 March 2011
title_short Anomalous TEC variations associated with the powerful Tohoku earthquake of 11 March 2011
title_full Anomalous TEC variations associated with the powerful Tohoku earthquake of 11 March 2011
title_fullStr Anomalous TEC variations associated with the powerful Tohoku earthquake of 11 March 2011
title_full_unstemmed Anomalous TEC variations associated with the powerful Tohoku earthquake of 11 March 2011
title_sort anomalous tec variations associated with the powerful tohoku earthquake of 11 march 2011
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2012-05-01
description On 11 March 2011 at 14:46:23 LT, the 4th largest earthquake ever recorded with a magnitude of 9.0 occurred near the northeast coast of Honshu in Japan (38.322<sup>°</sup> N, 142.369<sup>°</sup> E, Focal depth 29.0 km). In order to acknowledge the capabilities of Total Electron Content (TEC) ionospheric precursor, in this study four methods including mean, median, wavelet transform, and Kalman filter have been applied to detect anomalous TEC variations concerning the Tohoku earthquake. The duration of the TEC time series dataset is 49 days at a time resolution of 2 h. All four methods detected a considerable number of anomalous occurrences during 1 to 10 days prior to the earthquake in a period of high geomagnetic activities. In this study, geomagnetic indices (i.e. <i>D</i><sub>st</sub>, <i>K</i><sub><i>p</i></sub>, <i>A</i><sub><i>p</i></sub> and <i>F</i>10.7) were used to distinguish pre-earthquake anomalies from the other anomalies related to the geomagnetic and solar activities. A good agreement in results was found between the different applied anomaly detection methods on TEC data.
url http://www.nat-hazards-earth-syst-sci.net/12/1453/2012/nhess-12-1453-2012.pdf
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