TY - JOUR
T1 - Precursory enhancement of EIA in the morning sector
T2 - Contribution from mid-latitude large earthquakes in the north-east Asian region
AU - Ryu, Kwangsun
AU - Oyama, Koh Ichiro
AU - Bankov, Ludmil
AU - Chen, Chia Hung
AU - Devi, Minakshi
AU - Liu, Huixin
AU - Liu, Jann Yenq
N1 - Funding Information:
This work was supported by Mitsubishi Foundation Grant in Japan and partly supported by the Institutional Research Grant of SaTReC (Satellite Technology Research Center), at KAIST (Korea Advanced Institute of Science and Technology) in Korea. H. Liu is supported by JSPS KAKENHI Grant Numbers 15K05301, 15H02135, and 15H03733. The authors would like to thank Dr. M. Parrot and Dr. J. P. Lebreton at LPC2E/CNRS for developing and providing DEMETER ISL data. The space weather data were obtained from the OMNI data center ( http://omniweb.gsfc.nasa.gov ). In addition, the earthquake data were acquired from the USGS–NEIC data center ( http://earthquake.usgs.gov/regional/neic ).
PY - 2016/1/1
Y1 - 2016/1/1
N2 - To investigate whether the link between seismic activity and EIA (equatorial ionization anomaly) enhancement is valid for mid-latitude seismic activity, DEMETER observations around seven large earthquakes in the north-east Asian region were fully analyzed (M⩾6.8). In addition, statistical analysis was performed for 35 large earthquakes (M⩾6.0) that occurred during the DEMETER observation period. The results suggest that mid-latitude earthquakes do contribute to EIA enhancement, represented as normalized equatorial N e , and that ionospheric change precedes seismic events, as has been reported in previous studies. According to statistical studies, the normalized equatorial density enhancement is sensitive and proportional to both the magnitude and the hypocenter depth of an earthquake. The mechanisms that can explain the contribution of mid-latitude seismic activity to EIA variation are briefly discussed based on current explanations of the geochemical and ionospheric processes involved in lithosphere–ionosphere interaction.
AB - To investigate whether the link between seismic activity and EIA (equatorial ionization anomaly) enhancement is valid for mid-latitude seismic activity, DEMETER observations around seven large earthquakes in the north-east Asian region were fully analyzed (M⩾6.8). In addition, statistical analysis was performed for 35 large earthquakes (M⩾6.0) that occurred during the DEMETER observation period. The results suggest that mid-latitude earthquakes do contribute to EIA enhancement, represented as normalized equatorial N e , and that ionospheric change precedes seismic events, as has been reported in previous studies. According to statistical studies, the normalized equatorial density enhancement is sensitive and proportional to both the magnitude and the hypocenter depth of an earthquake. The mechanisms that can explain the contribution of mid-latitude seismic activity to EIA variation are briefly discussed based on current explanations of the geochemical and ionospheric processes involved in lithosphere–ionosphere interaction.
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U2 - 10.1016/j.asr.2015.08.030
DO - 10.1016/j.asr.2015.08.030
M3 - Article
AN - SCOPUS:84941591502
SN - 0273-1177
VL - 57
SP - 268
EP - 280
JO - Advances in Space Research
JF - Advances in Space Research
IS - 1
ER -