“…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…”