Data from a pulse-propagation experiment are analyzed to quantify fluctuati
ons in the transmitted acoustic signal. In the experiment a bottom-moored,
broadband source having a 460-Hz center frequency transmitted 273 km away t
o a bottom-moored, vertical hydrophone array spanning 180 m of the water co
lumn. pulses were transmitted every 12 min for a total duration of nearly 1
00 h. Because the minimal hydrophone separation at the receiving array was
less than 2 m, vertical behavior on small scales could be observed. Further
more, the vertical position of the receiving array enabled an examination o
f the near-caustic portion of wavefronts, and in some cases, the caustics t
hemselves. Unfortunately, because instrument motion measurements were unsuc
cessful, relative rather than absolute signal fluctuations were the princip
al observable in this analysis. (C) 1999 Acoustical Society of America. [S0
001-4966(99)01706-3].