Oceanographic variability creates a weak random propagation medium for acou
stic waves. The impact on acoustic transmission is becoming increasingly ap
preciated as the deterministic modelling of sound propagation in the ocean
has become tractable and better understood. Beyond the near field (where ph
ase fluctuations are weak) and the far field (where the scintillation index
becomes saturated) multiple-scattering theory predicts that random focusin
g will greatly enhance the acoustic energy density over small volumetric re
gions, which we call 'ribbons'. In 1985 an experiment was carried out in th
e eastern Mediterranean to test this prediction using acoustic propagation
along distinct, resolvable ray paths. This experiment is one of the few to
map the spatial structure of acoustic intensity with such a large vertical
aperture, and as far as the authors are aware it remains the only experimen
t to attempt to detect the two-dimensional structure of the predicted focus
ed ribbons for individual energy paths. Renewed impetus to publish the resu
lts has been provided by the recent focus on moderate- to high-frequency ac
oustics in near-shore and shallow-water environments. The experiment is des
cribed and high-intensity regions consistent with the theoretical predictio
ns are reported. A 3.5 kHz pulsed signal was transmitted over ranges of 11-
23 km and sampled over a vertical aperture of 250-350 m and horizontal aper
tures of 4.5 km. The acoustic signals travelling along individual ray paths
developed randomly focused regions of 6-18 dB over regions with a vertical
dimension of about 20 m and whose horizontal length could possibly be up t
o 1 km. The understanding of these features allows system limitations to be
estimated quantitatively and opens up the way to their constructive tactic
al use. The results are applicable to many systems from towed array sonars
to high-frequency bathymetric sidescan and minehunting.