Measurements with an array of low-frequency microphones are compared to ray calculations, describing the long range propagation of acoustic energy from the shock cone of the Concorde SST. This energy is ducted between the surface and the strong sound velocity gradient of the upper stratosphere. The measured pressure signatures are composed of one to five distinct wave groups arriving over a period of minutes; the number and sequence of arrivals is different for the Dulles-bound and JFK-bound airplanes. With respect to arrival time and azimuth of phase propagation, we find close correspondence between the highest amplitude wave groups and the refracted arrival predicted by ray calculations. Subsidiary wave groups apparently result from the diffracted ’’ground’’ wave and from volume scattering of acoustic energy into shadow zones.