Numéro
J. Phys. IV France
Volume 04, Numéro C5, Mai 1994
3ème Congrés français d'acoustique
3rd French conference on acoustics
Page(s) C5-1273 - C5-1276
DOI https://doi.org/10.1051/jp4:19945282
3ème Congrés français d'acoustique
3rd French conference on acoustics

J. Phys. IV France 04 (1994) C5-1273-C5-1276

DOI: 10.1051/jp4:19945282

The ambient noise energy motion in the near-surface layer in ocean wave-guide

V.A. SHCHUROV, V.I. ILYICHEV and V.P. KULESHOV

Pacific Oceanological Institute, Far Eastern Branch, Russian Academy of Sciences, 43 Baltiyskaya Str., Vladivostok, 690041, Russia


Abstract
The results of measurements of scalar - vector characteristics of the ambient noise acoustic field in deep ocean areas over the range of 1-800 Hz are presented. The subject of investigations were the ambient noise energy in the part of the ocean wave-guide that lied between the surface and the underwater sound channel axis lying at the depth of the order of 1200 m. A telemetric drifting autonomous system with combined receivers was used in the investigations. A combined receiver consisted of a scalar receiver (hydrophone) and a vector receiver of three components particle velocity. Our studies revealed that ambient noise energy transport in the vertical plane occurred in three main directions : 1) over the range of 1-12 Hz it proceeded from the underwater sound channel axis to the ocean surface in the angles range of 0°-30° ; 2) over the range of 32-141 Hz it proceeded from the sea surface to the underwater sound channel axis in the angles range of 0°-40° ; 3) over the range of 282-800 Hz noise energy flux made an angle between 10° and 30° with z axis, and its horizontal component coincided with wind wave propagation direction over the range of 447-800 Hz. Over the range of 282-355 Hz horizontal component of the noise energy flux coincided with ripple direction and over the range of 562-800 Hz it did with the propagation direction of wind surface waves.



© EDP Sciences 1994