The incident internal-wave ray has equation . Intersecting it with the bottom givesIts distance to the slope is consequentlyThe subcritically reflected ray rises through the same vertical distance at angle , so its next free-surface reflection is at
On the first leg, viscous attenuation of an internal-wave beam multiplies the energy density by . The bottom reflection multiplies it by and changes the wavenumber to . Since the corresponding Reynolds number is , attenuation on the second leg contributes . Ignoring boundary-layer enhancement as requested,
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