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- W2473922622 abstract "When obliquely observed from an airplane, gray clouds near the horizon are sometimes observed to overlap with white clouds. Photographic observation from an airplane and simulations using a three-dimensional radiative transfer model are conducted to understand why such clouds appear gray. From observations, the brightness depression rate of gray clouds relative to surrounding whitish clouds is about 25%, whereas in simulations, it is as high as about 30%. Conditions necessary for the observation of gray clouds are as follows: (1) two clouds at different altitudes do not overlap, but the higher cloud overlaps with the lower cloud along the line of sight when these clouds are observed in near-horizontal direction, and (2) the higher cloud is optically thin in the vertical direction, but optically thick along the line of sight." @default.
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- W2473922622 date "2016-07-19" @default.
- W2473922622 modified "2023-09-24" @default.
- W2473922622 title "Physical interpretation of gray cloud observed from airplanes" @default.
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- W2473922622 doi "https://doi.org/10.1364/ao.55.005761" @default.
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