The interaction between an internal gravity wave and turbulence in the stably-stratified nocturnal boundary layer.

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Abstract

Observations have been made of a stably-stratified nighttime boundary layer perturbed by Kelvin-Helmholtz internal waves with critical levels around 600 m. Significant turbulence intensities were measured although the time-mean gradient Richardson numbers were large and positive. It is shown by constructing energy budgets of wave and turbulent components separately that there is an essential flow of kinetic energy from wave to turbulence and that the mechanics of this exchange process depend upon the nonlinear character of the wave field.-from Authors

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Finnigan, J. J., Einaudi, F., & Fua, D. (1984). The interaction between an internal gravity wave and turbulence in the stably-stratified nocturnal boundary layer. Journal of the Atmospheric Sciences, 41(16), 2409–2436. https://doi.org/10.1175/1520-0469(1984)041<2409:TIBAIG>2.0.CO;2

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