Paper
19 November 2012 Lidar remote sensing of atmospheric aerosol and cloudiness: Monte Carlo modeling
Author Affiliations +
Proceedings Volume 8526, Lidar Remote Sensing for Environmental Monitoring XIII; 85260N (2012) https://doi.org/10.1117/12.977241
Event: SPIE Asia-Pacific Remote Sensing, 2012, Kyoto, Japan
Abstract
The light haze of a ground-based impulse LIDAR in an altitude-wise optically inhomogeneous cloud-free atmosphere was computed in dependence of various optical-geometrical parameters of the experiment using the Monte Carlo method. Modeling of the LIDAR echo-signal reflected off the lower boundary of a liquid droplet cloud for a ground-based LIDAR and off the upper boundary of the cloud for an aircraft- and space-based LIDAR was also completed. A feature of these calculations is the choice of the model with altitude-wise statistically inhomogeneous structure of aerosol scattering parameters as the optical model of a cloudless atmosphere. The echo-signals from clouds were computed in the assumption of statistical variation of the altitudes of the lower and upper cloudiness boundaries. In the calculations new effective discrete-stochastic modifications of local estimates were employed.
© (2012) COPYRIGHT Society of Photo-Optical Instrumentation Engineers (SPIE). Downloading of the abstract is permitted for personal use only.
Evgeniya Kablukova, Arseny B. Kargin, and Boris A. Kargin "Lidar remote sensing of atmospheric aerosol and cloudiness: Monte Carlo modeling", Proc. SPIE 8526, Lidar Remote Sensing for Environmental Monitoring XIII, 85260N (19 November 2012); https://doi.org/10.1117/12.977241
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KEYWORDS
Atmospheric modeling

Clouds

Scattering

Aerosols

Atmospheric particles

LIDAR

Atmospheric optics

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