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- W2055361154 abstract "Coordinated observations with lidar and balloon‐borne particle counters were used to characterize polar stratospheric clouds and to estimate a particle index of refraction. The index of refraction was estimated from comparisons of calculated and measured scattering ratios at a wavelength of 532 nm. The clouds, measured from McMurdo Station, Antarctica (78°S), were observed above 11 km at temperatures below 198 K and were divided into three classes based on their scattering properties and particle size. Clouds with a low scattering ratio, high depolarization, and significant fraction of particles with radii of >2.0 μm had a mean index of refraction of 1.42±0.04 and a mode of 1.43. Clouds with a moderate scattering ratio, low depolarization, and fewer particles of >2.0 μm, had a mean index of refraction of 1.39±0.03 and a mode of 1.37. Ice clouds, apparent from measurements of high scattering ratio, high depolarization, and high concentrations of particles of >1.0 μm, had a mean index of refraction of 1.32±0.02 and a mode of 1.31. Measurements in volcanic aerosol indicated a mean index of 1.43±0.04." @default.
- W2055361154 created "2016-06-24" @default.
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- W2055361154 date "1995-12-20" @default.
- W2055361154 modified "2023-10-01" @default.
- W2055361154 title "Polar stratospheric clouds and volcanic aerosol during spring 1992 over McMurdo Station, Antarctica: Lidar and particle counter comparisons" @default.
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- W2055361154 doi "https://doi.org/10.1029/95jd02029" @default.
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