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作 者:Weiping Jiang Yifang Ma Hongfei Liu Liansheng Deng Xiaohui Zhou
机构地区:[1]Research Center of GNSS,Wuhan University [2]Administration of Surveying,Mapping and Geoinformation of Yunan Province,Yunan Province Administration of Surveying,Mapping and Geoinformation [3]School of Geodesy and Geomatics,Wuhan University
出 处:《Earthquake Science》2013年第3期259-265,共7页地震学报(英文版)
基 金:supported by the National Natural Science Foundation of China(41074022);the National 863 Program of China(2012AA12A209);Open Research Fund Program of Geospace Environment and Geodesy(LOGEG),Ministry of Education,China(No.1202012)
摘 要:Vertical total electron content (VTEC) time series were obtained from 22 GPS stations near the epicenter of the Lushan earthquake. In this paper, we have adopted a sliding average method to detect and analyze anomalous VTEC associated with the earthquake. The results show that signif- icant, negative ionosphere VTEC anomalies appeared over the 5 days before the earthquake, and on the day when earthquake occurred. The maximum value of VTEC anoma- lies that exceeded the lower bound reached 20 TECU. The spatial distribution of VTEC anomalies showed a conjugate structure, which shifted to the magnetic equator, and subse- quently moved westwards.Vertical total electron content (VTEC) time series were obtained from 22 GPS stations near the epicenter of the Lushan earthquake. In this paper, we have adopted a sliding average method to detect and analyze anomalous VTEC associated with the earthquake. The results show that signif- icant, negative ionosphere VTEC anomalies appeared over the 5 days before the earthquake, and on the day when earthquake occurred. The maximum value of VTEC anoma- lies that exceeded the lower bound reached 20 TECU. The spatial distribution of VTEC anomalies showed a conjugate structure, which shifted to the magnetic equator, and subse- quently moved westwards.
关 键 词:Lushan earthquake Vertical totalelectron content (VTEC) Anomalous perturbationGPS
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