Published online by Cambridge University Press: 04 July 2016
Detailed measurements of atmospheric-turbulence velocity have been made by a specially instrumented aircraft at altitudes below one thousand feet over a variety of terrains. These measurements are analysed in terms of power-spectral-density and a statistical-discrete-gust model. To a good approximation, spatial increments in turbulence velocity are shown to satisfy scaling laws implying self-similarity for amplitudes up to about four times their root-mean-square value and over a wide range of scales. A three-parameter relationship is established between two parameters from the statistical-discrete-gust analysis, corresponding respectively to intermittency and gust intensity, and one from the power-spectral representation, related to the average rate of energy dissipation.