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