摘要
基于GPS数据对2015年尼泊尔M W7.8地震引起的同震电离层扰动进行统计与FFT频谱分析,探究地震电离层TEC扰动传播的时空特性。结果表明,震后5 min起出现明显的TEC扰动异常现象,持续时间超过6 min,呈现增大-减小-增大的变化趋势;扰动由震中向东、东北等方向传播,速率分别为2336.36 m/s和455.52~937.64 m/s;扰动的中心频率为3~7 mHz,符合瑞利波与声波引发的扰动频段。
In this paper,we calculate the ionospheric TEC disturbance caused by the 2015 M W7.8 Nepal earthquake and analyze the FFT spectrum based on GPS observation data to research temporal and spatial characteristics of earthquake ionospheric TEC.The results show that obvious abnormal disturbance appears 5 minutes after earthquake and lasts more than 6 minutes with a trend of increasing-decreasing-increasing.The disturbance propagates towards east,northeast and several directions,whose velocities are 2336.36 m/s and 455.52-937.64 m/s.The center frequencies are mostly 3-7 mHz,which is consistent with the disturbance spectrum caused by Rayleigh wave and acoustic wave.
作者
马玉
祝芙英
MA Yu;ZHU Fuying(Key Laboratory of Earthquake Geodesy,Institute of Seismology,CEA,40 Hongshance Road,Wuhan 430071,China)
出处
《大地测量与地球动力学》
CSCD
北大核心
2020年第9期957-961,969,共6页
Journal of Geodesy and Geodynamics
基金
中国地震局地震研究所和中国地震局地壳应力研究所基本科研业务费专项(IS201926303)
国家重点研发计划(2018YFC1503502)
亚太空间合作组织地震研究二期项目(WX0519502)。