Paper
22 September 1983 Visible And Infrared Extinction And Precipitation Rate In Falling Snow
Mary Ann Seagraves
Author Affiliations +
Proceedings Volume 0414, Optical Engineering for Cold Environments; (1983) https://doi.org/10.1117/12.935871
Event: 1983 Technical Symposium East, 1983, Arlington, United States
Abstract
Visible and infrared extinction in falling snow as observed by conventional transmissometers has shown a spectral dependence such that extinction increases with increasing wavelength in the absence of coexisting fog. Explanations of this wavelength dependence are given and techniques for modeling visible and infrared transmittance through falling snow are discussed. The spectral dependence may be used in the remote sensing of mass concentration and precipitation rate of falling snow.
© (1983) COPYRIGHT Society of Photo-Optical Instrumentation Engineers (SPIE). Downloading of the abstract is permitted for personal use only.
Mary Ann Seagraves "Visible And Infrared Extinction And Precipitation Rate In Falling Snow", Proc. SPIE 0414, Optical Engineering for Cold Environments, (22 September 1983); https://doi.org/10.1117/12.935871
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Cited by 1 scholarly publication.
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KEYWORDS
Particles

Transmittance

Infrared radiation

Visible radiation

Diffraction

Scattering

Atmospheric particles

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