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The angles from part (i) have sinesBy Snell law for elastic and acoustic waves, $\sin {\theta }_f/{\alpha }_f=\sin {\theta }_P/\alpha$. Both angles lie in $[0,\pi /2)$, so ${\theta }_f={\theta }_z$. The outgoing fluid ray tilts away from the inward-tilted normal by exactly its tilt from vertical; it therefore travels vertically upwards. This is hyperbolic interface collimation of P-waves.

The source-to-interface distance satisfiesOne can verify this by squaring, using $D^2-s^2=d^2{R}^2$. ConsequentlyAdding the vertical fluid travel time from the interface to height $z$ givesThus surfaces of equal arrival time in the fluid are horizontal planes. Their leading wave amplitude may vary with $R$: a planar wavefront does not imply a spatially uniform plane-wave solution at every order.

The spherical source potential $f(t-r/\alpha )/r$ gives leading longitudinal displacement field $-f^{\prime }(t-r/\alpha )/(\alpha r)$. Apply the local solid-fluid P-wave transmission coefficient to its potential at a smooth interface. In hyperbolic interface collimation of P-waves, transmitted rays are parallel, so ray-tube conservation for a P-wave jump makes the leading coefficient constant along each vertical ray. This yields the displayed jump for the first nonzero derivative discontinuity of the waveform. Smooth transverse derivatives multiply $f$ rather than $f^{\prime }$ and are one order more regular. The construction presupposes the indicated one-sided derivative jump exists; a source smooth to every order may have no jump.