Cloud weather

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  • A cloud is an aerosol consisting of a visible mass of minute liquid droplets, frozen crystals, or other particles suspended in the atmosphere of a planetary body.[1] Water or various other chemicals may compose the droplets and crystals. On Earth, clouds are formed as a result of saturation of the air when it is cooled to its dew point, or when it gains sufficient moisture usually in the form of water vapor from an adjacent source to raise the dew point to the ambient temperature. They are seen in the Earth`s homosphere which includes the troposphere, stratosphere, and mesosphere. Nephology is the science of clouds, which is undertaken in the cloud physics branch of meteorology.
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adjacent aerosol air ambient atmosphere body chemicals compose consisting cooled crystals dew droplets earth form formed frozen gains homosphere includes its liquid mass may mesosphere minute moisture other particles planetary point raise result saturation seen source stratosphere sufficient suspended temperature troposphere usually vapor various visible water which

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