Abstract
An attempt is made, for an anticyclonic stable situation in the atmospheric boundary layer during November 1978, to estimate the dissipation length. The turbulent dissipation and the turbulent kinetic energy, as measured on a 100 m high mast, exhibit large variability, due to the sporadic turbulent structure of the stable layer, and associated variability of the Richardson number. A comparison with different parameterizations of the turbulent dissipation rate allows a validation of these parameterizations.
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European Centre for Medium Range Weather Forecasts, Reading, England (work done while visiting scientist at CRPE).
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Louis, J.F., Weill, A. & Vidal-Madjar, D. Dissipation length in stable layers. Boundary-Layer Meteorol 25, 229–243 (1983). https://doi.org/10.1007/BF00119538
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DOI: https://doi.org/10.1007/BF00119538