GPS detection of the coseismic ionospheric disturbances following the 12 May 2008 M7.9 Wenchuan eart

• 作 者: SONG Qian DING Feng YU Tao WAN WeiXing NING BaiQi LIU LiBo ZHAO BiQiang
• 机 构: National Center for Space Weather,China Meteorological Administration,Key Laboratory of Earth and Pl
• 出 处: Science China(Earth Sciences)
• 发表日期: 2015年01期
• 关键词: epicenter waveform directional winds disturbance gravity excited receivers filte

Here we report two cases of coseismic ionospheric disturbances observed through a GPS network in China after the great Wenchuan earthquake at 06:28 UT on 12 May,2008.One is detected 7.9 min after the earthquake and had an intensive“N”shape oscillated waveform with a pronounced amplitude of about 1 TECU,which propagates approximately southward to the distance about 1000 km with the horizontal phase velocity of 600±84 m/s and the period of 9.5±1.3 min.The other is detected8.5 min after the earthquake and has an oscillated waveform more like a positive pulse with an amplitude of about 0.5 TECU,which propagates eastward to the distance about 800 km with the horizontal phase velocity of 720±59 m/s and the period of7.4±0.8 min.These two coseismic ionospheric disturbances are caused by the acoustic gravity waves excited by partial transformation of the acoustic waves originated from the energy release of the earthquake,somewhere near the epicenter.The directional preferences of these two coseismic ionospheric disturbances may be associated with the oblique geomagnetic field lines and the background winds filtering effect.

Here we report two cases of coseismic ionospheric disturbances observed through a GPS network in China after the great Wenchuan earthquake at 06:28 UT on 12 May, 2008.One is detected 7.9 min after the earthquake and had an intensive “N” shape oscillated waveform with a pronounced amplitude of about 1 TECU, which propagates approximately southward to the distance about 1000 km with the horizontal phase velocity of 600 ± 84 m / s and the period of 9.5 ± 1.3 min.The other is detected 8.5 min after the earthquake and has an oscillated waveform more like a positive pulse with an amplitude of about 0.5 TECU, which propagates eastward to the distance about 800 km with the horizontal phase velocity of 720 ± 59 m / s and the period of 7.4 ± 0.8 min These two coseismic ionospheric disturbances are caused by the acoustic gravity waves excited by partial transformation of the acoustic waves originated from the energy release of the earthquake, somewhere near the epicenter.The directional preferences of these tw o coseismic ionospheric disturbances may be associated with the oblique geomagnetic field lines and the background winds filtering effect.