Abstract
Analyses of lidar returns can be used for the calculation of micrometeorological parameters.1 From these measurements, the atmospheric diffusion parameters can also be calculated.
Here, we discuss the evaluation of these parameters directly from the lidar returns without deriving first the wind speed values. This is done by observing the temporal variation of eddy sizes of natural aerosol concentrations during unstable conditions.
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T. J. Swissler and M. Osborn
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