Spectral emission lines created in the solar chromosphere - corona tra
nsition region show Doppler shifts indicating widespread plasma down-f
lows. It has been proposed that this may be the result of the return o
f spicular material. We simulate a spicule numerically using the rebou
nd shock model and find that the resulting hydrodynamic evolution lead
s to a perceived up-flow in transition region spectral lines even thou
gh the average velocity in the line forming region is directed downwar
d. The explanation for this apparent paradox is found in the correlati
on between density and velocity in the waves generated by the rebound
shock 'spicule'.