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Multiple scattering of light in a turbid medium increases effective absorption of light by extending the pathlengths of photons in the medium. This enhances a low absorption of red light by ice and makes deep crevasses in snow, which radiate mostly multiple-scattered light, appear bluish (for example, Bohren CF 1987). The snow in the photo also appears bluish in the shadows. Is multiple-scattering of light in the snow an appropriate explanation of this blue color? (Hint: The photo was taken on a cloudless day!) Comments
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Topics in Particle and Dispersion Science (TPDSci) is an online publication (ISBN 0-9780628-0-9) intended to provide a concise review of interdisciplinary topics in the particle and particle dispersion science, with the emphasis on the most recent developments. It is extensively cross-referenced and can be accessed via several convenient threads:
TPDSci accepts brief original contributions and contributions that review and comment on publications within the scope of TPDSci.
This publication is available freely for a limited time.
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