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• W2177404949 abstract "Abstract A thermistor chain towed from 140° to 110°W along the equator revealed the presence of high-frequency internal waves in the upper 125 m having zonal wavelengths of 150–250 m. Turbulence dissipation rates, e, observed from a free-falling profiler were high when wave packets were present. Unfortunately, the frequency of the vertical profiles of e taken did not resolve the internal wave cycle, so a dynamical link between the waves and the mixing could not be directly observed with vertical profiler data. It is presumed that either wave-induced shear instability or advective instability destabilized the waves and led to increased e. The thermistor data, which were sampled at 20 Hz or approximately 12.5 cm horizontally, resolved part of the inertial subrange of turbulence and are used to determine the structure of turbulence within an internal wave cycle. A temperature gradient variance method for estimating e relies on a fully resolved Batchelor spectrum that, for this experiment, would have required..." @default.
• W2177404949 created "2016-06-24" @default.
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• W2177404949 date "1999-12-01" @default.
• W2177404949 modified "2023-09-29" @default.
• W2177404949 title "Mixing Structure of High-Frequency Internal Waves in the Upper EasternEquatorial Pacific" @default.
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• W2177404949 doi "https://doi.org/10.1175/1520-0485(1999)029<3090:msohfi>2.0.co;2" @default.
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