Abstract
The index of refraction and its short-term variations have been measured on a 152-m meteorological tower at three fixed levels and on a moveable platform. Analysis of the data reveals that the time rates of production and dissipation of refractivity fluctuations are approximately in balance under a variety of meteorological conditions, and that changes in the rate of dissipation usually coincide with comparable changes in the rate of production. Under reasonably stationary conditions, terms corresponding to the rate of change and vertical diffusion of refractivity variance are found to be negligible. Power spectral densities of the variations increase when the rate of generation (and dissipation) increase, and conversely. Comparison of the results with simultaneous acoustic sounder returns provides a valuable insight into the mechanisms responsible for changes in the rates of production and dissipation.
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Mandics, P.A. Generation and dissipation of microwave refractive-index fluctuations in the boundary layer. Boundary-Layer Meteorol 4, 311–322 (1973). https://doi.org/10.1007/BF02265240
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DOI: https://doi.org/10.1007/BF02265240