how different types of clouds are formed?
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Clouds Form in Different Ways As it rises, its pressure and temperature drop causing water vapor to condense. Eventually, enough moisture will condense out of the air to form a cloud. Several types of clouds form in this way including cumulus, cumulonimbus, mammatus, and stratocumulus clouds.
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The foundation consists of 10 major cloud types. In addition to cirrus, stratus, cumulus, and nimbus clouds, there are cirrostratus, cirrocumulus, altostratus, altocumulus, stratocumulus, nimbostratus, and cumulonimbus clouds. The following table places these cloud types into the four major cloud groups.
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From what I can tell, they are formed when there's rising air that creates wide-spread cloud cover, together with wind shear that blows across the rising air. This can set up gravity waves, where air moves up and down as buoyancy and gravity battle it out, creating long rippling waves that carry the clouds up and down.
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There are five types of weather: sunny, cloudy, windy, snowy, and rainy. It is described as the sun shining and giving warmth to the land. There are little to no presence of clouds. Cold temperatures and wind, however, will also be present on some areas of the earth.
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Almost all rain is produced from low-level clouds. Stratus clouds produce steady rains, and cumulus clouds produce intense, stormy precipitation.
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All in all, there are ten fundamental types of clouds. Often, you'll some places simply class clouds as cirrus, stratus, and cumulus because these clouds are the most common and representative for each altitude class. High-level clouds (5-13 km): cirrocumulus, cirrus, and cirrostratus.
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Cumulonimbus clouds are menacing looking multi-level clouds, extending high into the sky in towers or plumes. More commonly known as thunderclouds, cumulonimbus is the only cloud type that can produce hail, thunder and lightning.
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Thus, the 10 types are: Low-level clouds (cumulus, stratus, stratocumulus) that lie below 6,500 feet (1,981 m) Middle clouds (altocumulus, nimbostratus, altostratus) that form between 6,500 and 20,000 feet (1981–6,096 m) High-level clouds (cirrus, cirrocumulus, cirrostratus) that form above 20,000 feet (6,096 m)
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While it's true that clouds contain water, they actually aren't made of water vapor. ... The air around us is partially made up of invisible water vapor. It's only when that water vapor cools and condenses into liquid water droplets or solid ice crystals that visible clouds form.
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A rainbow cloud occurs because of something called cloud iridescence. It usually happens in altocumulus, cirrocumulus, lenticular and cirrus clouds. It is the same basic concept as a rainbow: small water droplets or small ice crystals within the cloud scatter the Sun's light. You've probably seen a rainbow before.
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Normally, cumulus clouds produce little or no precipitation, but they can grow into the precipitation-bearing congestus or cumulonimbus clouds. Cumulus clouds can be formed from water vapour, supercooled water droplets, or ice crystals, depending upon the ambient temperature.
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How do nimbostratus clouds form? Nimbostratus clouds form through the deepening and thickening of an altostratus cloud, often along warm or occluded fronts. These clouds extend through the lower and mid-layers of the troposphere bringing rain to the surface below.
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['Low-level clouds (cumulus, stratus, stratocumulus) that lie below 6,500 feet (1,981 m)', 'Middle clouds (altocumulus, nimbostratus, altostratus) that form between 6,500 and 20,000 feet (1981–6,096 m)', 'High-level clouds (cirrus, cirrocumulus, cirrostratus) that form above 20,000 feet (6,096 m)']
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['High cloud - cirrus, cirrocumulus, cirrostratus.', 'Middle cloud - altostratus, altocumulus, nimbostratus.', 'Low cloud - stratus, stratocumulus.', 'Vertical - cumulus, cumulonimbus.']
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High-level clouds (5-13 km): cirrocumulus, cirrus, and cirrostratus. Mid-level clouds (2-7 km): altocumulus, altostratus, and nimbostratus. Low-level clouds (0-2 km): stratus, cumulus, cumulonimbus, and stratocumulus.
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The Short Answer: Clouds are created when water vapor, an invisible gas, turns into liquid water droplets. These water droplets form on tiny particles, like dust, that are floating in the air. You hang up a wet towel and, when you come back, it's dry.
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When warm moist air meets colder drier air, the warm air rises, the water vapor condenses in the air, and forms a cloud. As the water vapor condenses it releases heat, which is a form of energy. ... As the thunderstorm progresses, eventually the rain cools the entire process down and the energy is gone.