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- W1154594530 abstract "This chapter reviews kinetic energy dissipation observed in the upper ocean. Observations of vertical temperature microstructure at Ocean Station P were made with a freely falling tethered microstructure recorder. Two storms were observed during the MILE experiment, and during the second milder storm temperature gradient fluctuations were resolved to the smallest dissipative scales in more than 90% of the data. The temperature gradient profiles were broken into blocks approximately 60 cm in vertical extent and spectrally analyzed with a fast Fourier transform. A cut-off wavenumber was found for each spectrum, and a Batchelor scale was determined from the cut-off wavenumber; a detailed description of this method of calculation of the Batchelor scale is described in the chapter." @default.
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- W1154594530 date "1980-01-01" @default.
- W1154594530 modified "2023-09-27" @default.
- W1154594530 title "Kinetic Energy Dissipation Observed in the Upper Ocean" @default.
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- W1154594530 doi "https://doi.org/10.1016/s0422-9894(08)71214-5" @default.
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