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- W86689889 abstract "Direct measurements of the turbulent structure of a benthic, tidal boundary layer have been made by recording several time series of simultaneous horizontal and vertical velocity fluctuations at various distances above the bottom. For the duration of the experiment the layer thickness 5 was approximately 5 m and the mean current speed ranged between 50 and 120 cm sec -1 Velocities were sampled each second for approximately four hours. Analysis of the experimental data indicates that the velocity fluctuations were statistically separable into two main components, (1) large-scale, quasi-ordered structures which are primarily responsible for vertical momentum transport, and (2) a background of relatively isotropic turbulence of smaller scale. The frequency of occurrence of the large, coherent structures was found to be somewhat dependent on tidal phase. In general, the period between such events scales on the outer flow variables U∞ δ* in a manner analogous to the bursting phenomenon observed in laboratory experiments. The intermittency of the vertical momentum transport associated with these large-scale structures is shown to be a limiting factor in the accuracy of direct measurements of Reynolds stress in such natural, shear flows." @default.
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- W86689889 date "1977-01-01" @default.
- W86689889 modified "2023-09-26" @default.
- W86689889 title "Turbulent Structure in a Benthic Boundary Layer" @default.
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- W86689889 doi "https://doi.org/10.1016/s0422-9894(08)70834-1" @default.
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