Intermittent periods of high momentum transport have been measured in a tidal boundary layer (Reϑ ≈ 2.6×105). The data have been interpreted in terms of the bursting phenomenon reported in laboratory experiments. The experimental period between bursts is consistent with that predicted by T ≈ kδ*/U∞ where k is the displacement thickness, and U∞ is the stream velocity outside the boundary layer.
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C.M. Gordon (1975) studied this question.