The effect of atmospheric scattering and ground reflection upon the determination of the height of the night airglow
作者:
Edward V. Ashburn,
期刊:
Journal of Geophysical Research
(WILEY Available online 1954)
卷期:
Volume 59,
issue 1
页码: 67-70
ISSN:0148-0227
年代: 1954
DOI:10.1029/JZ059i001p00067
数据来源: WILEY
摘要:
Chandrasekhar's theory of radiative transfer was used to calculate the effect of atmospheric scattering and ground reflection upon the determination of the height of the night airglow when the extinction coefficient is 0.15. It was found that the atmospheric scattering is a significant factor, but that the ground reflection is not important except for high albedo (snow cover).
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