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- W2028292073 abstract "Laplace’s tidal equation is derived from the differential equation which governs the inertial oscillations of an incompressible fluid, in the limit of small h/a , where h denotes the depth of ocean and a the radius of the Earth. The vertical acceleration is not neglected explicitly. It is shown that when we apply the condition of the vanishing of the component of velocity normal to the ocean bottom and of the vanishing of the pressure at the surface of the ocean, the differential equation of inertial oscillations can be reduced to Laplace’s tidal equation in the limit of small h/a ." @default.
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- W2028292073 title "A derivation of Laplace’s tidal equation from the theory of inertial oscillations" @default.
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- W2028292073 doi "https://doi.org/10.1098/rspa.1975.0090" @default.
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