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    Lidar Sensing of Plume Dispersion: Analysis Methods and Product Quality for Light-Scattering Tracer Particles 

    Source: Journal of Atmospheric and Oceanic Technology:;1987:;volume( 004 ):;issue: 004:;page 674
    Author(s): Eberhard, W. L.; McNice, G. T.; Troxel, S. W.
    Publisher: American Meteorological Society
    Abstract: Analysis procedures are described for retrieving accurate plume information from lidar data on light-scattering particles during atmospheric dispersion experiments. Interactive computer graphics aided in the solution of ...
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    Some Microphysical Properties of an Ice Cloud from Lidar Observation of Horizontally Oriented Crystals 

    Source: Journal of Applied Meteorology:;1978:;volume( 017 ):;issue: 008:;page 1220
    Author(s): Platt, C. M. R.; Abshire, N. L.; McNice, G. T.
    Publisher: American Meteorological Society
    Abstract: Lidar observations of a winter ice cloud in the zenith gave a very high reflection but a very small depolarization. When the lidar was tilted more than 0.5° away from the zenith, the reflection amplitude fell to 3% of it's ...
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    Depolarization of Lidar Returns from Virga and Source Cloud 

    Source: Journal of Applied Meteorology:;1976:;volume( 015 ):;issue: 011:;page 1200
    Author(s): Derr, V. E.; Abshire, N. L.; Cupp, R. E.; McNice, G. T.
    Publisher: American Meteorological Society
    Abstract: The observed depolarization of polarized lidar signals scattered from virga and a source cloud may be interpreted to show that the source cloud is largely glaciated, and the virga is composed of ice crystals not randomly ...
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