The Characteristics of Magnetic Signals Observed at Lulin ELF Station and Their Association with Earthquakes in Taiwan

Electromagnetic wave data from years 2009 - 2010 which were recorded by the extremely-low-frequency (ELF) station at Lulin Observatory in Taiwan (120.87°E, 23.46°N; 2862 m) are analyzed to explore the wave properties and their association with seismic and geomagnetic activities. Specifically, the po...

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Main Authors: Shao-Ming Ho, Kaiti Wang, Alfred B. C. Chen, Han-Tzong Su, Sung-Ming Huang, Ruei-Ron Hsu, Tung-Shin Hsu
Format: Article
Language:English
Published: Springer 2013-01-01
Series:Terrestrial, Atmospheric and Oceanic Sciences
Subjects:
Online Access: http://tao.cgu.org.tw/images/attachments/v242p197.pdf
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author Shao-Ming Ho
Kaiti Wang
Alfred B. C. Chen
Han-Tzong Su
Sung-Ming Huang
Ruei-Ron Hsu
Tung-Shin Hsu
author_facet Shao-Ming Ho
Kaiti Wang
Alfred B. C. Chen
Han-Tzong Su
Sung-Ming Huang
Ruei-Ron Hsu
Tung-Shin Hsu
author_sort Shao-Ming Ho
collection DOAJ
description Electromagnetic wave data from years 2009 - 2010 which were recorded by the extremely-low-frequency (ELF) station at Lulin Observatory in Taiwan (120.87°E, 23.46°N; 2862 m) are analyzed to explore the wave properties and their association with seismic and geomagnetic activities. Specifically, the power spectra, the ellipticity and the orientation of the below-10-Hz wave signals are studied. The correlation coefficients of these ELF signals and geomagnetic activity indices Dst and Kp are within -0.2 to 0.2, indicating geomagnetic activities are not likely sources for these emissions. In the frequency versus time (f-t) spectrograms, a few events exhibit a frequency shift between 4 and 6 Hz and the possible association with seismic activities of magnitudes (M) larger than 4 in the vicinity of Taiwan are examined. The subset of earthquakes in Taiwan with M/r2 (r is the epicenter distance in kilometer from the Lulin station) of greater than 6 × 10-4, a total number of 50, show a higher association with ELF wave events showing a frequency down-shift within 7 days prior to the earthquakes and a frequency bounce-back within 7 days after the earthquakes. The epicenters of these earthquakes are all within a distance of 100 km from the Lulin station and with a depth of 50 km, suggesting that the detected ELF frequency-shift wave events maybe are pre-earthquake electromagnetic signals.
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spelling doaj.art-3738aae75778446cb251bd9340f747462022-12-22T00:47:01ZengSpringerTerrestrial, Atmospheric and Oceanic Sciences1017-08392311-76802013-01-0124219710.3319/TAO.2012.09.19.01(SEC)1123The Characteristics of Magnetic Signals Observed at Lulin ELF Station and Their Association with Earthquakes in TaiwanShao-Ming HoKaiti WangAlfred B. C. ChenHan-Tzong SuSung-Ming HuangRuei-Ron HsuTung-Shin HsuElectromagnetic wave data from years 2009 - 2010 which were recorded by the extremely-low-frequency (ELF) station at Lulin Observatory in Taiwan (120.87°E, 23.46°N; 2862 m) are analyzed to explore the wave properties and their association with seismic and geomagnetic activities. Specifically, the power spectra, the ellipticity and the orientation of the below-10-Hz wave signals are studied. The correlation coefficients of these ELF signals and geomagnetic activity indices Dst and Kp are within -0.2 to 0.2, indicating geomagnetic activities are not likely sources for these emissions. In the frequency versus time (f-t) spectrograms, a few events exhibit a frequency shift between 4 and 6 Hz and the possible association with seismic activities of magnitudes (M) larger than 4 in the vicinity of Taiwan are examined. The subset of earthquakes in Taiwan with M/r2 (r is the epicenter distance in kilometer from the Lulin station) of greater than 6 × 10-4, a total number of 50, show a higher association with ELF wave events showing a frequency down-shift within 7 days prior to the earthquakes and a frequency bounce-back within 7 days after the earthquakes. The epicenters of these earthquakes are all within a distance of 100 km from the Lulin station and with a depth of 50 km, suggesting that the detected ELF frequency-shift wave events maybe are pre-earthquake electromagnetic signals. http://tao.cgu.org.tw/images/attachments/v242p197.pdf EarthquakesExtremely-low-frequency (ELF) disturbancesPre-cursor signal
spellingShingle Shao-Ming Ho
Kaiti Wang
Alfred B. C. Chen
Han-Tzong Su
Sung-Ming Huang
Ruei-Ron Hsu
Tung-Shin Hsu
The Characteristics of Magnetic Signals Observed at Lulin ELF Station and Their Association with Earthquakes in Taiwan
Terrestrial, Atmospheric and Oceanic Sciences
Earthquakes
Extremely-low-frequency (ELF) disturbances
Pre-cursor signal
title The Characteristics of Magnetic Signals Observed at Lulin ELF Station and Their Association with Earthquakes in Taiwan
title_full The Characteristics of Magnetic Signals Observed at Lulin ELF Station and Their Association with Earthquakes in Taiwan
title_fullStr The Characteristics of Magnetic Signals Observed at Lulin ELF Station and Their Association with Earthquakes in Taiwan
title_full_unstemmed The Characteristics of Magnetic Signals Observed at Lulin ELF Station and Their Association with Earthquakes in Taiwan
title_short The Characteristics of Magnetic Signals Observed at Lulin ELF Station and Their Association with Earthquakes in Taiwan
title_sort characteristics of magnetic signals observed at lulin elf station and their association with earthquakes in taiwan
topic Earthquakes
Extremely-low-frequency (ELF) disturbances
Pre-cursor signal
url http://tao.cgu.org.tw/images/attachments/v242p197.pdf
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