Differential Doppler compression and travel time of individual peaks i
n the arrival sequence (relative to an overall average) are measured f
or the 5500-km acoustic transmissions from a moving source at Heard Is
land to Christmas (Crab) Island, The differentials cannot be explained
by simple adiabatic propagation models. A hybrid theory, coupling pol
ar and temperate models at the Antarctic Front, can account for some o
f the qualitative features. Differential Doppler could be a useful too
l for identifying ray arrivals.