“…In both deep ocean and shallow water continental shelf environments, a major source of acoustic field scintillation is internal waves [7,8,9]. Early efforts to describe signal scintillation statistics in the ocean were based on multipath theory, with the resultant field being the sum of multiple random phase components [10,11,12]. The instantaneous received signal therefore has an exponential distribution for intensity or a Rayleigh distribution for amplitude [10,11,12], and a 5.6 dB intensity standard deviation [11].…”