Use the spatial internal-wave ray tracing model, with , and reflect the rays so that the frequency and tangential wave number are preserved. At a vertical wall the horizontal energy direction reverses; at a horizontal wall the vertical energy direction reverses. On the sloping wall the reflection depends on internal-wave slope criticality. The three-reflection orbit below encounters that wall at a height above , so the wall reverses the horizontal energy direction there.
First take the packet to leave the bottom upward and to the left, with . The four segments of the loop areThe left-wall reflection is at and the top reflection at . The slope intersection solves , giving the internal-wave ray return mapThus the next formal bottom reflection is at . On , the slope heights are between approximately and , consistent with the assumed reflection type.
An internal-wave attractor is a stable periodic ray, so solve . This gives , and thereforeThe successive vertices areThis is clockwise circulation in the plane. Differentiating the internal-wave ray return map showsNeighbouring bottom intersections converge to the periodic orbit, geometrically focusing the energy beam.
For completeness, the opposite upward launch direction has the reversed three-reflection itinerary: slope, top, left. In the interval where this itinerary is valid, putThe three-reflection reverse map is , with domain . Its fixed point is the same, but . Counterclockwise packets defocus from that orbit. Except for the exactly periodic reverse ray, they eventually leave this itinerary. In the full geometric reflection construction, omitted-side or additional-slope reflections redirect generic rays into the clockwise attracting branch. Tangency and exactly critical reflections are singular exceptions requiring finite-wavelength or dissipative treatment.
Clockwise spatial internal-wave attractor and convergence of neighbouring ray loops in the trapezoidal basin
. The bottom reflection is a formal spatial-ray idealization: part (b) shows that the WKB approximation itself fails near , so the diagram does not imply arrival and reflection there in finite WKB travel time. In a real fluid, viscous attenuation of an internal-wave beam, finite wavelength, internal-wave breaking and ensuing turbulence and mixing limit the beam width and energy density. Unlimited focusing is a property of the ideal geometric model, not a prediction for the resolved physical wave.
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