In the summer of 1991, sound propagation and reverberation experiments were
carried out in the Yellow Sea. Explosive sound sources and omnidirectional
hydrophones were used. The sound speed profile consisted of a warmer surfa
ce isovelocity layer, a strong thermocline and a cooler isovelocity bottom
layer. When both the source and the receiver were located above the thermoc
line, the transmission loss along a certain course and the non-directional
average reverberation intensity showed similar frequency-selective attenuat
ion at around 1300 Hz. On the basis of experimental results and some circum
stantial evidence, the authors believe that the observed frequency-selectiv
e attenuation is due to swimbladder-bearing fish (probably, anchovies) livi
ng only above the thermocline. (C) 1999 Academic Press.