Hydrodynamics and Sound

The energy equation for surface waves over an incompressible fluid like water subject to viscous dissipation is conveniently derived from Equation (1.5.12) in which ? = ? gz and ? = ? o. When quantities of third order and higher are discarded, we have
Let the waves propagate in the x direction and integrate the equation over the interior of a thin, vertical slice of fluid, aligned with the wave crests, of thickness ? x and of unit lateral span (Figure 5.2.1). For viscous flow the velocity v = ( ? x, 0, ? z) must vanish at the bottom z = ? h, and the stress-free condition at the free surface must be applied in the form ( p ? ij ? ? ij) n j ? pn i ? ? ij n j = 0 at z = ?, where ? z ? ? ?/ ? t. Retaining only second-order terms and considering the limit as ?x ? 0, we find
where
and
is the pressure reduced by the mean hydrostatic pressure ? ? o gz.
The wave energy E per unit surface area for the wave (5.1.11) on water of finite depth consists of kinetic energy T and potential energy Q, whose values we first calculate for the fluid region ABCD of Figure 5.2.2 beneath