Physical interpretation of gray cloud observed from airplanes

Rintaro Okamura, Hironobu Iwabuchi

Research output: Contribution to journalArticle

1 Citation (Scopus)

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.

Original languageEnglish
Pages (from-to)5761-5765
Number of pages5
JournalApplied optics
Volume55
Issue number21
DOIs
Publication statusPublished - 2016 Jul 20

ASJC Scopus subject areas

  • Atomic and Molecular Physics, and Optics
  • Engineering (miscellaneous)
  • Electrical and Electronic Engineering

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