Abstract
The optical constants of dried natural aerosol material obtained from rain and snow are determined over the spectral range 450–5000 cm−1 Constants were determined from the reflection spectrum by the Cramers-Kronig method. Results are presented graphically.
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Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Fizika, No. 11, pp. 11–14, November, 1983.
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Sonchik, V.K. Optical constants of natural aerosols in the IR region of the spectrum. Soviet Physics Journal 26, 973–975 (1983). https://doi.org/10.1007/BF00896652
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DOI: https://doi.org/10.1007/BF00896652