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中文核心期刊

1993年7月12日日本北海道地震次声波

Infrasound waves caused by earthquake on 12 July 1993 in Japan

  • 摘要: 1993年7月12日北京时间21点21分19秒在北京中关村次声接收阵上及时地发现并完整地记录了日本北海道地震所产生的当地次声波(包括地震纵波、横波、表面波所辐射的声波)和震中次声波。其中当地次声波分别有:周期为12s,振幅为0.8 Pa,持续3.4min;及周期为12s,振幅为0.4 Pa,持续1min和周期为30s,振幅为1.3 Pa,持续12min;震中次声波周期为137s,振幅为6.9 Pa,持续28min。它们叠加在周期为12min、幅度为10 Pa的大气异常现象的波列上。

     

    Abstract: Remarkable infrasound wave trains have been recorded at Beijing Infrasound Observatory at 21:21 BT (Beijing Time) on July 12,1993.It is a complete set of local waves (including primary wave,shear wave and Rayleigh waves) and epicenter infrasound waves caused by an earthquake in Japan.There are periods of 12 s,12 s,30 s,and amplitudes of 0.8 Pa,0.4 Pa,1.3 Pa,and durations of 3.4 min,1 min,12 min respectively.The epicenter infrasound waves have period of 137 s,and its maximum amplitude of 6.9 Pa and durations 28 min.They were superimposed on a much longer and more usual series of waves with period about 12 min and amplitude 10 Pa;such waves,which are of natural origin,are characteristically received during meteorological inversions.

     

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