On the use of acoustics for studying suspended oceanic sediment and for determining the onset of the shallow thermocline

John R Proni , Fred C Newman , Donna C Rona , David E Drake , George A Berberian , Charles A Lauter Jr. , Ronald L Sellers
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引用次数: 13

Abstract

Acoustic observations of a low-density sediment flow originating from a dredge operating in the main Miami shipping channel have been made. The flow proceeded seaward along layered thermal gradients at the top of the shallow thermocline and at greater depths. Acoustic, thermal, salinity, chemical, and transmissivity measurements were made during summer and winter in 1974.

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声学用于研究海洋悬浮沉积物和确定浅层温跃层的开始
对在迈阿密主要航道上作业的挖泥船产生的低密度沉积物流进行了声学观测。水流沿着浅层温跃层顶部和更深处的分层热梯度向海方向流动。声学、热、盐度、化学和透射率测量在1974年夏季和冬季进行。
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