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- W1985504251 abstract "Intriguing new observations from an ice camp, manned during the Cooperative Eastern Arctic Experiment (CEAREX) on the Northwest flank of the Yermak Plateau, indicate that ocean microstructure may be detectable with ‘‘standard’’ acoustic instrumentation (i.e., acoustic Doppler current profilers) of moderately high frequency (150–300 kHz). The strength of the CEAREX data set is the simultaneous observation of kinetic energy dissipation rate, temperature dissipation rate, and acoustic backscatter from both 160- to 300-kHz Doppler profilers. The turbulence levels observed during CEAREX were particularly strong (ε≳10−7 W kg−1) and occurred in well-defined patches. Backscattered intensity anomalies of 2 to 6 dB were found to be coincident in time and space with patches of strong turbulence in the thermocline. It is shown that the acoustic intensity anomalies co-vary with the strength of the turbulent dissipation above a threshold that presumably represents the background particulate scattering level. Theoretical predictions of the acoustic intensity level based on the microstructure measurements are used to support the hypothesis that the enhanced scattering levels are due to temperature anomalies." @default.
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- W1985504251 date "1992-04-01" @default.
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- W1985504251 title "Simultaneous observations of acoustic scattering and ocean microstructure in the arctic." @default.
- W1985504251 doi "https://doi.org/10.1121/1.403175" @default.
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