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Physical interpretation of gray cloud observed from airplanes
Applied Optics
|July 28, 2016
Summary
Gray clouds appear darker than white clouds due to specific atmospheric conditions. This phenomenon occurs when optically thin, higher clouds overlap lower clouds along the line of sight, reducing brightness by approximately 25-30%.
Area of Science:
- Atmospheric Science
- Cloud Physics
- Radiative Transfer
Background:
- Clouds are essential components of Earth's climate system.
- Cloud appearance, including color and brightness, is influenced by light scattering and absorption.
- The perception of cloud color can be complex, especially under varying observation angles.
Purpose of the Study:
- To investigate the reasons behind the observation of gray clouds appearing to overlap with white clouds.
- To understand the optical conditions that lead to a perceived brightness depression in clouds.
Main Methods:
- Utilized photographic observations from an airplane.
- Employed simulations with a three-dimensional radiative transfer model.
Main Results:
- Observed gray clouds exhibited a brightness depression rate of approximately 25% compared to surrounding whitish clouds.
- Simulations indicated a brightness depression rate as high as 30% under specific conditions.
- Identified two key conditions for observing gray clouds: (1) near-horizontal observation of an optically thin higher cloud overlapping a lower cloud, and (2) the higher cloud being optically thick along the line of sight.
Conclusions:
- The apparent grayness of clouds is a result of their optical properties and their relative positions and altitudes.
- The overlap of an optically thin, higher cloud with a lower cloud, when viewed obliquely, causes a significant brightness depression.
- Radiative transfer modeling supports observational findings, confirming the conditions necessary for gray cloud perception.
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