The liquid water density within a cumulus cloud has been found to change with height above the cloud base rather than being approximately constant throughout the cloud. These cloud streets cover vast areas and may be broken or continuous.
Viewed from below, this cloud usually has a horizontal base.
The concentration slowly dropped off as altitude increased to the height of the top of the cloud, where it immediately dropped to zero again.Cumulus clouds can form in lines stretching over 480 kilometres (300 mi) long called cloud streets. This is also the explanation for the unusual height of the humilis clouds. However, at the same time, they heat the earth by around 7 °C (13 °F) by reflecting emitted radiation, an effect largely caused by Cumulus clouds are a genus of free-convective low-level cloud along with the related limited-convective cloud stratocumulus.
On the other hand, clouds which display a ragged pattern, which is caused due to turbulence, are known as Cumulus fractus. Cumulus congestus clouds are much larger, look like caulilower, and are associated with bad weather. High clouds form 3,000 to 7,600 metres (9,800 to 24,900 ft) in high latitudes, 5,000 to 12,000 metres (16,000 to 39,000 ft) in temperate latitudes, and 6,100 to 18,000 metres (20,000 to 59,100 ft) in low, tropical latitudes.Altocumulus clouds are a mid-level cloud that forms from 2,000 metres (6,600 ft) high to 4,000 metres (13,000 ft) in polar areas, 7,000 metres (23,000 ft) in temperate areas, and 7,600 metres (24,900 ft) in tropical areas.A stratocumulus cloud is another type of stratocumuliform cloud. The other clouds in this level are cirrus and cirrostratus. In addition unlike the other cumulus types, they tend to have more of a grey tone that is due to the high concentration of water droplets. Cumulus clouds with a huge projection are known as Cumulus castellanus. Consequentially, since they develop immediately after the condensation level, they do not grow into other clouds, but rather dissipate in a matter of minutes. They form when Some cumuliform and stratocumuliform clouds have been discovered on most other planets in the solar system.
The cumulus humilis cloud structures are usually associated and known in meteorological circles as the fair weather clouds. Turbulence is generally moderate. Cumulus Humilis. However, sometimes, a phenomenon known as temperature inversion can take place. The cumulus humilis cloud structures are usually associated and known in meteorological circles as the fair weather clouds. Cumulus clouds are often precursors of other types of clouds, such as In this phase, water vapor condenses on various nuclei present in the air, forming the cumulus cloud. Cumulus humilis clouds are formed throughout the day as the sun rays fall on the ground and heat it. However, they are more common for summer, when the high temperatures permit the rise of the hot air masses from the oceans and landscapes. In the middle level are the alto- clouds, which consist of the limited-convective stratocumuliform cloud altocumulus and the stratiform cloud altostratus.
In general, when the fronts of warm air start raising up in the atmosphere the rules of physics indicate they are going to cool down with a certain number of degrees Celsius for each kilometer. Cumulus characterized by only a small vertical extent and appearing generally as if flattened.
The main reasons of their development are the small masses of hot air that rise from the earth's surface during summer. Regardless of whether they appear alone or with other clouds, they are associated with a clear and sunny weather, making them any aircraft pilotâs dream.
These clouds form from ground level to 2,000 metres (6,600 ft) at all latitudes. However, it is important to note that sometimes they can collapse into stratocumulus structures and will cover large areas of the sky. Below the cloud.
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