ESTIMATION OF THE MAIN SIZE OF ATMOSPHERIC ICE CRYSTALS USING THE COLOR RATIO IN LASER SENSING APPLICATION

The paper presents the dependences of the spectral ratio on the particle size for four shapes at six wavelengths. The study was conducted using the extended database of light scattering matrices of the IAO SB RAS, on data obtained within the physical optics approximation, for the case of random spatial orientation of particles and single scattering. Several particle shapes, which are typical for ice clouds, were studied at wavelengths of incident radiation from 0.355 to 2.150 μm. The results of this work can be used for interpretation of the lidar signal, in particular, to retrieve the size of atmospheric ice particles.

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Publication Details

Published
2025-06-21
DOI
https://doi.org/10.56820/conferencearticle_685d0a9f460e25.41216549
Primary Topic
Atmospheric aerosols and clouds
Type
article
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article

ESTIMATION OF THE MAIN SIZE OF ATMOSPHERIC ICE CRYSTALS USING THE COLOR RATIO IN LASER SENSING APPLICATION

D. Timofeev, Victor A. Shishko, Alexander V. Konoshonkin, Natalia V. Kustova et al.
Atmospheric aerosols and clouds
article

ESTIMATION OF THE MAIN SIZE OF ATMOSPHERIC ICE CRYSTALS USING THE COLOR RATIO IN LASER SENSING APPLICATION

D. Timofeev, Victor A. Shishko, Alexander V. Konoshonkin, Natalia V. Kustova, I. Tkachev
article en

Abstract

The paper presents the dependences of the spectral ratio on the particle size for four shapes at six wavelengths. The study was conducted using the extended database of light scattering matrices of the IAO SB RAS, on data obtained within the physical optics approximation, for the case of random spatial orientation of particles and single scattering. Several particle shapes, which are typical for ice clouds, were studied at wavelengths of incident radiation from 0.355 to 2.150 μm. The results of this work can be used for interpretation of the lidar signal, in particular, to retrieve the size of atmospheric ice particles.

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Atmospheric aerosols and clouds
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