Estimation of epicenter using an empirical relationship between epicentral distance and traveltime of the first arrival

초동 전파시간과 진앙거리의 경험적인 관계를 이용한 진앙 추정

  • 신동훈 (국립기상연구소 지구환경시스템연구팀) ;
  • 박창업 (서울대학교 지구환경과학부) ;
  • 황의홍 (기상청 지진정책담당관실) ;
  • 전영수 (국립기상연구소 지구환경시스템연구팀)
  • Published : 2007.06.07

Abstract

The classic graphical method to determine the epicenter uses differences between the arrival times of P and S waves at each station. In this research, a robust approach is proposed, which provides a fast and intuitive estimation of earthquake epicenters. This method uses an empirical relationship between epicentral distance and traveltime of the first arrival P phase of local or regional earthquake. The relationship enables us to estimate epicentral distances and draw epicentral circles from each station with P-traveltimes counted from a probable origin time. As the assigned time is getting close to the origin time of the earthquake, epicentral circles begin to intersect each other at a possible location of the epicenter. Then the possibility of the epicenter can be expressed by a function of the time and the space. We choose the location which gives the minimum standard deviation of the origin time as an estimated epicenter. In this research, 918 P arrival times from 84 events occurring from 2005 to 2006 listed in the KMA earthquake catalog are used to determine the empirical P-traveltime function of epicentral distances.

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