2015
DOI: 10.1016/j.oceaneng.2015.08.064
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Near- and far-field tsunami amplitudes by a moving curvilinear stochastic submarine slide shape based on linearized water wave theory

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Cited by 6 publications
(3 citation statements)
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“…The TUNAMI model operates using the nonlinear theory of the shallow water equation that is solved by a leap-frog and upwind scheme based on a cartesian coordinate system. The cartesian coordinate system is limited by a small area, with a small change in the spherical surface of the Earth 58 , 59 . We therefore modified the existing governing equation of the TUNAMI model to a geographic (spherical) coordinate system based on Baba et al 50 , as given in Eqs.…”
Section: Methodsmentioning
confidence: 99%
“…The TUNAMI model operates using the nonlinear theory of the shallow water equation that is solved by a leap-frog and upwind scheme based on a cartesian coordinate system. The cartesian coordinate system is limited by a small area, with a small change in the spherical surface of the Earth 58 , 59 . We therefore modified the existing governing equation of the TUNAMI model to a geographic (spherical) coordinate system based on Baba et al 50 , as given in Eqs.…”
Section: Methodsmentioning
confidence: 99%
“…All these studies neglected the nonlinear terms in the boundary conditions to study the generation of the tsunami waves using the transform methods. In this paper, an analytical approach was used to illustrate the tsunami wave, the L 2 norms of the free surface 55 elevation, the displaced water volume as a result of the bottom topography, the potential energy of the free surface elevation and the velocity flow rates in the open ocean during the generation and propagation processes for a given stochastic bottom profile ζ(x, y, t).The Laplace and Fast Fourier Transform (FFT) methods could be applied taken into account constant depths h. After applying the Fourier-Laplace transform of the Laplace equation (1) and the boundary conditions (2) - (4), and using the initial conditions in (5), the velocity potential ϕ ̅ ( k 1 , k 2 , z, s ) and the free surface elevation η ̅ (k 1 , k 2 , s ) are obtained, respectively as seen in Ramadan et al (2015) as: 5…”
Section: Mathematical Formulation Of the Linear Water Wave Problemmentioning
confidence: 99%
“…Submarine earthquakes are often represented as random phenomena, where white noise stochastic processes are 45 adopted to properly model their frequency content (Greco et al 2014). Numerous studies used Gaussian white noise stochastic processes to account the random components of bottom deformation in tsunami simulation, see (Omar et al 2012;Allam et al 2014;Ramadan et al 2015;Ramadan et al 2017). Dynamic bottoms are often used to model the waves generated by some type of bottom motion.…”
Section: Introductionmentioning
confidence: 99%