Abstract
We report here analysis of the first observations with a new instrument, ARIES, designed to record the acoustic backscatter from bubble clouds at several levels below the surface of the ocean. The instrument is deployed on a subsurface mooring and records internally. Data has been analysed from deployments of ARIES for one week in the Irish Sea and for periods of 4 and 9 weeks near the edge of the UK continental shelf, during periods in which meteorological data, waves, and near-surface temperatures and, on occasion, currents, were being recorded by other instruments. The results, while being generally similar to earlier measurements in coastal waters, show that the bubble clouds are more intense, having greater acoustic scattering cross per unit volume, Mv, and extend, on average, deeper into the water column. A simple model accounting for the shape of the clouds, their advection through the sonar beam, and their decay (through bubbles returning to the surface or through their gas dissolving int... Abstract We report here analysis of the first observations with a new instrument, ARIES, designed to record the acoustic backscatter from bubble clouds at several levels below the surface of the ocean. The instrument is deployed on a subsurface mooring and records internally. Data has been analysed from deployments of ARIES for one week in the Irish Sea and for periods of 4 and 9 weeks near the edge of the UK continental shelf, during periods in which meteorological data, waves, and near-surface temperatures and, on occasion, currents, were being recorded by other instruments. The results, while being generally similar to earlier measurements in coastal waters, show that the bubble clouds are more intense, having greater acoustic scattering cross per unit volume, Mv, and extend, on average, deeper into the water column. A simple model accounting for the shape of the clouds, their advection through the sonar beam, and their decay (through bubbles returning to the surface or through their gas dissolving int...

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