Dr. Palmer et al., RECEPTION AT ASCENSION OF THE HEARD ISLAND FEASIBILITY TEST TRANSMISSIONS, The Journal of the Acoustical Society of America, 96(4), 1994, pp. 2432-2440
At Ascension, about 9200 km from the source ship, all transmissions fr
om the Heard Island Feasibility Test were recorded on at least eight h
ydrophones and, for many transmissions, on 11 hydrophones. The depths
of most of these hydrophones are near the depth of the sound channel a
xis but some are considerably deeper. All are bottom mounted. Signal-t
o-noise ratios were found to be surprisingly high. Averaged over the c
ontinuous wave (cw) transmissions and in a l-Hz band, signal-to-noise
ratios for the axial hydrophones south of the island range from about
19 to 30 decibels (dB), adjusted to a source level of 220 dB (referenc
ed to 1 mu Pa at 1 m). The average signal-to-noise ratio for a hydroph
one at a depth approximately 0.8 km below the axis is about 16 dB, sug
gesting acoustic energy was not restricted to a narrow interval in dep
th centered about the sound channel axis as had been anticipated. The
travel time of the earliest arrival was found to be about 1 h, 44 min,
17 s. A late, scattered signal was observed for at least 23 min after
termination of the direct signal. An unexpected combination of phase
stability and amplitude variability was observed in the received signa
ls. Continuing analysis of the Ascension data set is likely to provide
considerable information about the characteristics of acoustic signal
s that have propagated global distances.