Journal of Korean Society of Coastal and Ocean Engineers (한국해안·해양공학회논문집)

Korean Society of Coastal and Ocean Engineers (한국해안·해양공학회)
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Development of a Numerical Model Considering Active Tsunami Generation

능동적 지진해일 생성을 고려한 지진해일 수치모형 개발

  • Jung, Taehwa (Department of Civil and Environmental Engineering, Hanbat National University) ;
  • Hwang, Sooncheol (School of Civil, Environmental, and Architectural Engineering, Korea University) ;
  • Son, Sangyoung (School of Civil, Environmental, and Architectural Engineering, Korea University)
  • 정태화 (한밭대학교 건설환경공학과) ;
  • 황순철 (고려대학교 건축사회환경공학부) ;
  • 손상영 (고려대학교 건축사회환경공학부)
  • Received : 2021.06.25
  • Accepted : 2021.07.20
  • Published : 2021.08.31
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Abstract

Seabed deformation due to the fault failure have both a spatial variation and temporal history. When the faulting process initiates at a certain point beneath seabed, the failure spreads out to neighboring points, resulting in temporal changes of deformation. In particular, such a process induces tsunami waves from the vertical motion of seabed. The uprising speed of seabed affects the formation of initial surface profile, eventually altering the arrival time and runup of tsunamis at the coast. In this work, we developed a numerical model that can simulate the generation and propagation of tsunami waves by considering the horizontal and vertical changes of seabed in an active and dynamic manner. For the verification of the model, it was applied to the 2011 Tohoku-oki earthquake in Japan and the results confirmed that the accuracy was improved compared to the existing passive and static model.

단층파괴에 의한 해저지형변화는 공간적으로 시간차를 가진다. 특정 지점에서 파괴가 발생하면 이웃지점으로 단층파괴가 전파하면서 시간차에 따른 단층파괴가 발생하며, 단층파괴시 연직방향으로 상승하면서 지진해일을 야기한다. 해저 지형의 상승속도는 지진해일 초기파형에 영향을 주며 결과적으로 지진해일의 도달시간 및 크기에 영향을 준다. 본 연구에서는 단층파괴에 의한 해저 지형의 수평적 및 수직적 변화를 능동적 및 동적으로 고려하여 지진해일의 생성 및 전파를 모의할 수 있는 수치모형을 개발하였다. 모델의 검증을 위하여 2011년 동일본대지진에 대해 적용하였으며 기존의 수동적 및 정적 모형에 비해 정확성이 개선되는 것을 확인하였다.

Keywords

References

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