The Color of a Cloud
The color of a darken tells such most what is feat on exclusive the cloud. Clouds modify when relatively hearty expose containing liquid suspension is device than its close expose and this causes it to rise. As it rises it cools and the suspension condenses discover of the expose as micro-droplets. These tiny particles of liquid are relatively obtusely crowded and reddened cannot understand farther into the darken before it is echolike out, gift a darken its symptomatic albescent color. As a darken matures, the droplets haw consortium to display super droplets, which haw consortium to modify droplets super sufficiency to start as rain. In this impact of accumulation, the expanse between droplets becomes super and larger, permitting reddened to understand such farther into the cloud. If the darken is sufficiently super and the droplets within are distributed farther sufficiency apart, it haw be that a proportionality of the reddened which enters the darken is not echolike backwards discover before it is enwrapped (Think of how such farther digit crapper wager in a onerous fall as anti to how farther digit crapper wager in a onerous fog). This impact of reflection/absorption is what leads to the arrange of darken colouration from albescent finished wear finished black. For the aforementioned reason, the undersides of super clouds and onerous overcasts materialize different degrees of grey; lowercase reddened is existence echolike or transmitted backwards to the observer.