• Ocean and Polar Research
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• 제29권1호
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• pp.9-31
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• 2007

Most seismic sea waves in the East Sea originate from earthquakes occurring near the Japanese west coast. While the waves propagate in the East Sea, they are deformed by refraction, diffraction and scattering. Though the Boussinesq equation is most applicable for such wave phenomena, it was not used in numerical modelling of seismic sea waves in the East Sea. To examine characteristics of seismic sea waves in the East Sea, numerical models based on the Boussinesq equation are established and used to simulate recent tsunamis. By considering Ursell parameter and Kajiura parameter, it is proved that Boussinesq equation is a proper equation for seismic sea waves in the East Sea. Two models based on the Boussinesq equation and linear wave equation are executed with the same initial conditions and grid size ($1min{\times}1min$), and the results are compared in various respects. The Boussinesq equation model produced better results than the linear model in respect to wave propagation and concentration of wave energy. It is also certified that the Boussinesq equation model can be used for operational purpose if it is optimized. Another Boussinesq equation model whose grid size is $40sec{\times}30sec$ is set up to simulate the 1983 and 1993 tsunamis. As the result of simulation, new propagation charts of 2 seismic sea waves focused on the Korean east coast are proposed. Even though the 1983 and 1993 tsunamis started at different areas, the propagation paths near the Korean east coast are similar and they can be distinguished into 4 paths. Among these, total energy and propagating time of the waves passing over North Korea Plateau(NKP) and South Korea Plateau(SKP) determine wave height at the Korean east coast. In case of the 1993 tsunami, the wave passing over NKP has more energy than the wave over SKP. In case of the 1983 tsunami, the huge energy of the wave passing over SKP brought about great maximum wave heights at Mukho and Imwon. The Boussinesq equation model established in this study is more useful for simulation of seismic sea waves near the Korean east coast than it is the Japanese coast. To improve understanding of seismic sea waves in shallow water, a coastal area model based on the Boussinesq equation is also required.

• 대한수학회논문집
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• 제13권4호
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• pp.889-901
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• 1998

Numerical approximations by pseudospectral method are obtained for the damped Boussinesq equation which is a modification of the good Boussinesq equation. The consistency and stability of the method are obtained using the extended Lax-Richtmyer equivalence theorem, which imply the convergence of the method. We obtain error estimates of O(h$^{s}$ ＋ k$^2$) for a fully discrete pseudospectral method.

• 대한수학회지
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• 제45권1호
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• pp.79-95
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• 2008

The local existence of solutions for the initial-boundary value problem of a generalized Boussinesq equation on the half line is considered. The approach consists of replacing he Fourier transform in the initial value problem by the Laplace transform and making use of modern methods for the study of nonlinear dispersive wave equation

• Journal of applied mathematics & informatics
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• 제8권1호
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• pp.45-57
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• 2001

A parametric scheme is proposed for the numerical solution of the nonlinear Boussinesq equation. The numerical method is developed by approximating the time and the space partical derivatives by finite-difference re placements and the nonlinear term by an appropriate linearized scheme. The resulting finite-difference method is analyzed for local truncation error and stability. The results of a number of numerical experiments are given for both the single and the double-soliton wave. AMS Mathematics Subject Classification : 65J15, 47H17, 49D15.

• Journal of applied mathematics & informatics
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• 제13권1_2호
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• pp.11-27
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• 2003

A fourth order in time and second order in space scheme using a finite-difference method is developed for the non-linear Boussinesq equation. For the solution of the resulting non-linear system a predictor-corrector pair is proposed. The method is analyzed for local truncation error and stability. The results of a number of numerical experiments for both the single and the double-soliton waves are given.

• 한국해안해양공학회지
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• 제13권4호
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• pp.296-308
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• 2001

Wei et al.의 완전비선형 Boussinesq방정식을 4차의 Adams predictorcorrector기법을 사용하여 차분하고 면 내부조파기법과 스폰지 경계충을 사용하였으며 쇄파구조를 추가하였다. 면 내부조파기법을 사용해 목적파를 잘 재현할 수 있었다. 비선형성이 부각되는 고립파의 천수실험을 통해 완전비선형 모형의 정화성을 확인할 수 있었고 해저평붕으로 인한 규칙파의 변형을 모의해 보았다. 쇄파 수치실험을 통해 적용된 쇄파구조의 특성을 확인해 보았고 수중천퇴에 대한 이차원 파랑전파 수치실험을 통해 비선형 모형의 중요성을 확인하였다.

• 대한수학회논문집
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• 제26권2호
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• pp.207-214
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• 2011

The formal linearization method is an efficient method for constructing multisoliton solution of some nonlinear partial differential equations. This method can be applied to nonintegrable equations as well as to integrable ones. In this paper, we obtain multisoliton solution of generalization Burger's equation and the (3+1)-dimension Burger's equation and the Boussinesq equation by the formal linearization method.

• 한국환경과학회지
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• 제11권1호
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• pp.57-61
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• 2002

To investigate the flow characteristics by the water stage variation between stream-aquifer, the new solution of nonlinear Boussinesq equation was derived and extended using the Boltzmann transformation. The soundness of the analytic solution obtained from this study was examined by the comparison with the linearized analytic solution and the numerical solution by finite difference method. And the movement, velocity, flowrate and volume of flow caused by the stage variation of stream and the existence of regional gradient were estimated. This new analytic solution can express the groundwater movement between stream-aquifer. So, it might be helpful to manage water environment.

• 한국해안해양공학회지
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• 제17권3호
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• pp.202-212
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• 2005

수중 천퇴 인근에 해양구조물을 설치하는 경우, 구조물에 작용하는 설계하중을 구하기 위하여 파고뿐만 아니라 천퇴 주변 파랑변형에 의하여 이차적으로 발생된 파랑류를 아울러 고려하여야 한다. 본 연구에서는 천퇴 주변의 파랑변형과 파랑류를 계산하기 위하여 비선형 Boussinesq방정식 모델과 선형 완경사방정식 모델을 각각 적용하였다. 대상 천퇴는 Vincent and Briggs(1989)의 수리실험에서와 동일하며 실험조건은 규칙파, 일방향 또는 다방향 불규칙파 입사를 포함하는 비쇄파조건으로 하였다. 두 수치모델은 공히 천퇴 중심선을 따라 파랑류가 대칭적으로 형성됨을 잘 보여주었다. 그리고 수리실험에서의 파고계측선을 따라 계산된 파고변화는 전체적으로 실험 결과와 잘 일치하였다.

• 한국해안해양공학회지
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• 제18권2호
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• pp.154-165
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• 2006

본 연구에서는 수중 천퇴부에서 쇄파가 발생할 시 주변 파랑과 파랑류의 평형계를 직접 해석할 수 있는 Boussinesq 방정식 모델을 수립하고 이 결과를 수리실험 결과와 비교하였다. 사용된 쇄파모델은 쇄파 감쇠항을 모멘텀 방정식에 포함시키는 일종의 와점성 계수 모델이며, 관련된 쇄파 매개변수의 적정 값들을 Vincent and Briggs (1989)의 규칙파 실험자료를 이용한 민감도 분석을 통하여 결정하였다. 구해진 적정 매개변수 값들을 가지고 수치해석을 수행하여 이 결과를 불규칙파 실험결과와 이어도 천연암초의 수리모형실험 결과와 비교하였다. 그 결과, 천퇴부 하류 쪽에 파 진행방향으로 향하는 강한 쇄파유도류가 발생함에 따라 저파고대가 형성되며 전반적으로 계측파고의 분포와 유사함을 확인하였다.