ASA 128th Meeting - Austin, Texas - 1994 Nov 28 .. Dec 02

2aAO16. Change of sound ray by various equations of the sound velocity in the 621-km propagation experiment.

Toshio Tsuchiya

Toshiyuki Nakanishi

Yasutaka Amitani

Hiroshi Ochi

Hidetoshi Fujimori

Deep-Sea Technol. Dept., Japan Marine Sci. and Technol. Ctr., 2-15 Natsushima-cho, Yokosuka 237, Japan

Akio Hasegawa

Natl. Defense Acad. of Japan, 1-10 Hashirimizu, Yokosuka 239, Japan

Generally, sound velocity used to be calculated according to equations by Wilson (1960), DelGrosso (1974), Chen and Millero (1977), and others, which were obtained by direct measurement in laboratories based on water depth, temperature, and salinity data collected by the XBT (expendable Bathey-tharmograph) or CTD (conductivity temperature depth) system. However, in observations such as ocean acoustic tomography (OAT) where it is necessary to make accurate measurement of the sound wave propagation time over the distance of hundreds to thousands of kilometers, even the slightest difference of the sound velocity can produce significant errors in the observatory accuracy. Thus the effect of various equations of the sound velocity on the formation of the specific sound ray in the SOFAR channel was examined by using the simulation method by the sound ray theory. The simulation results were compared with the specific sound ray data obtained in the 621-km propagation experiment in the northeast Pacific Ocean, and as a result, the equation by Chen and Millero is found to be the most consistent among the three equations.