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| navigate by keyword : above adjacent aerosol ambient atmosphere body1 branch chemicals cloud clouds comprising cooled crystals droplets earth earths form formed from frozen gains homosphere includes liquid made mass mesosphere meteorology minute moisture nephology particles physics planetary point raise result saturation science seen source stratosphere sufficient surface suspended temperature they troposphere undertaken usually vapor various visible water when which |
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| In meteorology, a cloud is an aerosol comprising a visible mass of minute liquid droplets, frozen crystals, or particles suspended in the atmosphere above the surface of a planetary body.[1] The droplets and crystals may be made of water or various chemicals. 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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Stockphotos.ro (c) 2026. All stock photos are provided by Dreamstime and are copyrighted by their respective owners. |
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