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General
Cloud cover Cloud physics Cloud types High-clouds (Family A) Cirrocumulus Cirrus cloud Cirrostratus Middle-clouds (Family B) Altostratus Altocumulus Low-clouds (Family C) Cumulus cloud Stratocumulus cloud Nimbostratus cloud Stratus cloud |
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![]() .In mountainous areas one often finds the peaks above the clouds as seen here with the Piz Bernina in the Swiss Alps.^
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![]() Clouds and cloud bow above the Pacific Ocean.
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![]() Rain clouds over the North Sea taken from the coast of Herne Bay, Kent.
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![]() Lenticular cloud over Wyoming.
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| The
Cloud disambiguation |
| This is a disambiguation page, which lists works which share the same title. If an article link referred you here, please consider editing it to point directly to the intended page. |
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[[File:|thumb|right|200px|Clouds in the sky]] A cloud is water in the atmosphere (air) that we can see. It is where rain and snow comes from.
Water on the earth evaporates (turns into gas) and goes up into the sky. There, when it is colder, the water condenses: it changes from a gas to drops of water or crystals of ice. We see these drops of water as clouds. The drops fall back down to earth as rain, and then the water evaporates again. This is called the "water cycle".
Clouds on other planets are sometimes just collections of gases.
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The atmosphere always has a little bit of water vapor that humans can not see. Clouds form when the atmosphere can no longer hold all the invisible air vapor.[1] Any more water vapor condenses into very small water drops.[1]
Warm air holds more of water vapor than cool air.[1] So if warm air with lots of water inside cools, it can form a cloud. These are ways air can cool enough to form clouds:
Clouds are heavy. The water in a cloud can have a mass of several million tons. Every cubic metre (m3) of the cloud has only about 5 grams of water in it. Cloud droplets are also about 1000 times heavier than evaporated water, so they are much heavier than air. They do not fall, but stay in the air, because there is warm air all round the heavier water droplets. When water changes from gas to droplets, this makes heat. Because the droplets are very small, they "stick" to the warm air.
Sometimes, clouds appear to be brilliant colors at sunrise or sunset. This has shown to be due to pollution in the air.
]] Clouds are classified according to how high the base of the cloud is in the sky.[1] This system was suggested in 1802.
High clouds will form from 10,000 and 25,000 ft (3,000 and 8,000 m) in cold places, 16,500 and 40,000 ft (5,000 and 12,000 m) in the temperate regions and 20,000 and 60,000 ft (6,000 and 18,000 m) in the very hot tropics.[2]
Middle clouds usually form at 6,500 ft (2,000 m). However, they may form as high as 13,000 ft (4,000 m), 23,000 ft (7,000 m) or 25,000 ft (8,000 m). It depends on where they are. Nimbostratus clouds are sometimes included with the middle clouds.[2]
They are sometimes on ground level.[1] They can also be discovered up to 6,500 ft (2,000 m)[2] high. They include the strato clouds.[1] Cumulo clouds are also low-level and are made up of water drops.[1] When they push up through higher levels they also have ice crystals. These are found up to and include the stratus (dense and grey). When stratus clouds contact the ground, they are called fog.
Low-level clouds include:[3]
There are different sorts of cloud, because of how fast the air goes up and if the air stands still or is moving. Also, some clouds make more rain, or make thunder and lightning. These differences come from how big the water droplets are, and how they join together.
There are three basic types of clouds:[1]
Clouds from
Clouds and cloud bow above the Pacific Ocean. |
In the Bible, clouds are often a sign of God's presence.
Dictionary definitions from Wiktionary
Textbooks from Wikibooks
Quotations from Wikiquote
Source texts from Wikisource
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News stories from Wikinews
bjn:Rakun (météorologi)krc:Булутfrr:Swarken
Here are sentences from other pages on Cloud, which are similar to those in the above article.
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