Put and seek the slowly attenuating wave envelope in
At order , the equation gives the internal gravity wave dispersion relation
At order , retaining one derivative of the slowly varying amplitude gives
Using therefore yields
Hence the leading viscous attenuation of an internal-wave beam is
The wave energy density, being quadratic in the amplitude, decays twice as rapidly in the exponent.
The incident internal-wave ray has equation . Intersecting it with the bottom gives
Its distance to the slope is consequently
The 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,