NASA NTRS ยท 19820056692
Lidar clear atmosphere multiple scattering dependence on receiver range
Abstract
The degree of multiple scattering encountered by nadir-directed lidar in clear atmosphere conditions was assessed by the Monte Carlo method based on a model of the vertical distribution of aerosol scattering in the atmosphere. The lowest 3 km of the atmosphere were regarded as containing 90% of the aerosol optical thickness, with the unity normalized value for the forward peak of the aerosol phase function being 4.38 at a 694.3 nm laser wavelength. Results were obtained for two lidar receiver heights for three receiver field of view (FOV) angular halfwidths. An increase in receiver height was determined to cause a significant increase in the amount of angular scattering of the lidar signal. A factor of 20 change in receiver height produced an order of magnitude change in the single to multiple scattering ratio.
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Spinhirne, J. D.. 1982-07-15. Lidar clear atmosphere multiple scattering dependence on receiver range. https://ntrs.nasa.gov/citations/19820056692
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