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This paper is concerned with a Cauchy-Poisson problem in a weakly stratifiedocean of uniform finite depth bounded above by an inertial surface (IS). Theinertial surface is composed of a thin but uniform distribution ofnoninteracting materials. The techniques of Laplace transform in time andeither Green's integral theorem or Fourier transform have been utilized in themathematical analysis to obtain the form of the inertial surface in terms ofan integral. The asymptotic behaviour of the inertial surface is obtained forlarge time and distance and displayed graphically. The effect ofstratification is discussed

Waves due to initial disturbances at the inertial surface in a stratified fluid of finite depth