c what are cumulus clouds made of
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What Are Cumulus Clouds Made Up Of? Clouds can seem like a very abstract part of nature. Authors even use imagery of a mass of dark billowing clouds on the horizon to represent some unforeseen threat looming just out of human perception. In reality, the presence of clouds is a much more scientific phenomenon. There are three main varieties of clouds: cirrus, cumulus and stratus. They are made when air rises because of heat, the shape of the landscape or a weather front and is cooled as it reaches higher altitudes. Cumulus clouds are made of different states of water and air. Thermals
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Temperature The high cloud group consists of Cirrus, Cirrostratus, and Cirrocumulus clouds. High clouds are made of ice crystals due to the cold air in the upper sky. The base of a high cloud above the surface can ...more.
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Cumulonimbus cloud Cumulonimbus, from the Latin cumulus (heap) and nimbus (rainstorm, storm cloud), is a dense towering vertical cloud associated with thunderstorms and atmospheric instability, forming from water vapor carried by powerful upward air currents.umulonimbus can form alone, in clusters, or along cold front squall lines. These clouds are capable of producing lightning and other dangerous severe weather, such as tornadoes. Cumulonimbus progress from overdeveloped cumulus congestus clouds and may further develop as part of a supercell.
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Cloud Cumuliform cloudscape over Swifts Creek, Australia. In meteorology, a cloud is an aerosol comprising a visible mass of minute liquid droplets or frozen crystals, both of which are made of water or various chemicals. The droplets or particles are suspended in the atmosphere above the surface of a planetary body. On Earth, clouds are formed by the saturation of air in the homosphere (which includes the troposphere, stratosphere, and mesosphere). The air may be cooled to its dew point by a variety of atmospheric processes or it may gain moisture (usually in the form of water vapor) from an adjacent source.
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Types of Clouds Cumulus clouds are white, puffy clouds that look like pieces of floating cotton. Cumulus clouds are often called fair-weather clouds. The base of each cloud is flat and the top of each cloud has rounded towers.
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Cumulus Clouds When several cumulonimbus clouds occur beside each other, forming a line, they become what is known as a “squall”. Another type of cumulus cloud is the altocumulus cloud. These are much smaller clouds, looking like individual little cotton balls up in the sky.
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- Cumulo-means heap or pile in Latin. Cumulus clouds are often described as puffy, cotton-like or fluffy in appearance, and have flat bases. Cumulus clouds, being low-level clouds, are generally less than 1,000 m (3,300 ft) in altitude unless they are the more vertical cumulus congestus form.Cumulus clouds may appear by themselves, in lines, or in clusters.umulus clouds, being low-level clouds, are generally less than 1,000 m (3,300 ft) in altitude unless they are the more vertical cumulus congestus form.
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Cumulonimbus Cumulonimbus clouds belong to the Clouds with Vertical Growth group. They are generally known as thunderstorm clouds. A cumulonimbus cloud can grow up to 10km high. At this height, high winds will flatten the top of the cloud out into an anvil-like shape. Cumulonimbus clouds are associated with heavy rain, snow, hail, lightning, and tornadoes.
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Types of Clouds Cumulus clouds are puffy clouds that sometimes look like pieces of floating cotton. The base of each cloud is often flat and may be only 1000 meters (3300 feet) above the ground. The top of the cloud has rounded towers. When the top of the cumulus resembles the head of a cauliflower, it is called cumulus congestus or towering cumulus. These clouds grow upward, and they can develop into a giant cumulonimbus, which is a thunderstorm cloud.
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- Clouds formed by vertical currents in unstable air are cumulus meaning accumulation or heap; they are characterized by their lumpy, billowy appearance. Clouds formed by the cooling of a stable layer are stratus meaning stratified or layered; they are characterized by their uniform, sheet-like appearance.
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New Haven, CT Weather Temperature variations between night and day tend to be moderate during summer with a difference that can reach 20 degrees Fahrenheit, and fairly limited during winter with an average difference of 18 degrees Fahrenheit. The annual average precipitation at New Haven is 52.73 Inches. Rainfall in is fairly evenly distributed throughout the year. The wettest month of the year is May with an average rainfall of 4.70 Inches.
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- Cumulonimbus, from the Latin cumulus (heap) and nimbus (rainstorm, storm cloud), is a dense towering vertical cloud associated with thunderstorms and atmospheric instability, forming from water vapor carried by powerful upward air currents. cumulonimbus calvus: cloud with puffy top, similar to cumulus congestus which it develops from; under the correct conditions in can become a cumulonimbus capillatus. 2  cumulonimbus capillatus: cloud with cirrus-like, fibrous-edged top.
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Types of Clouds Cumulus clouds are often called fair-weather clouds. The base of each cloud is flat and the top of each cloud has rounded towers. When the top of the cumulus clouds resemble the head of a cauliflower, it is called cumulus congestus or towering cumulus.irrostratus clouds are thin, sheetlike high clouds that often cover the entire sky. They are so thin that the sun and moon can be seen through them. Cirrostratus clouds usually come 12-24 hours before a rain or snow storm. Cirrocumulus clouds appear as small, rounded white puffs that appear in long rows.
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How to Predict the Weather using Clouds Cirrus Clouds are high altitude, wispy clouds, seen in fine weather. Cirrostratus Clouds are made up of ice particles and form a halo around the sun. If a Cirrus filled sky darkens and turns to Cirrostratus it is a sign of rain or snow, depending on temperature. Altostratus Clouds form a greyish veil over the sun or moon. If they get darker and thicken, it is a sign that rain is on the way. Nimbostratus Clouds form low blankets of cloud and indicate rain or snow, lasting for several hours. Stratocumulus Clouds can form a lumpy mass covering the entire sky and may produce light rain, but usually dissipate by the late afternoon or evening. Stratus Clouds are low clouds that form a fog like layer and may produce drizzle.
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Cumulus cloud Cumulo-means heap or pile in Latin. Cumulus clouds are often described as puffy, cotton-like or fluffy in appearance, and have flat bases. Cumulus clouds, being low-level clouds, are generally less than 1,000 m (3,300 ft) in altitude unless they are the more vertical cumulus congestus form. Cumulus clouds may appear by themselves, in lines, or in clusters.
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Different Types of Clouds Cumulus clouds look like fluffy tufts of cotton floating in the sky. Sometimes they might take the shape of a dragon, a turtle or some other creature. Cumulonimbus clouds are large, flat clouds that spread across the sky. One end of the cloud might be shaped like an anvil.
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Cumulonimbus cloud Well-developed cumulonimbus clouds are characterized by a flat, anvil-like top (anvil dome), caused by wind shear or inversion near the tropopause. The shelf of the anvil may precede the main cloud's vertical component for many miles, and be accompanied by lightning.
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- The following Cities are next to Leeds, AL: 1  Birmingham is 13.6 miles west of Leeds, AL. 2  Trussville is 6.7 miles north of Leeds, AL. 3  Irondale is 5.5 miles west of Leeds, AL.  Moody is 5.5 miles northeast of Leeds, 1  AL. Dunnavant is 3.3 miles southeast of Leeds,  AL.
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- Cirrus (Ci) Cirrus clouds are composed mainly of ice crystals due to their height in the atmosphere (6000 m, 20,000 ft and above). The dryness of the air higher in the atmosphere contributes to their thin, wispy look.
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Cirrocumulus cloud Cirrocumulus is one of the three main genus-types of high-altitude tropospheric clouds, the other two being cirrus and cirrostratus. They usually occur at an altitude of 5 kilometres (16,000 ft) to 12 kilometres (39,000 ft). Like lower altitude cumuliform and stratocumuliform clouds, cirrocumulus signifies convection.hus cirrocumulus clouds are usually short-lived. They usually only form as part of a short-lived transitionary phase within an area of cirrus clouds and can also form briefly as a result of the breaking up of part of a cumulonimbus anvil.
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High clouds Latin: cirrus-lock or tuft of hair; cumulus-heap. Cirrocumulus clouds are lots of small white clouds-called cloudlets-grouped together at high levels. Composed almost entirely from ice crystals, the little cloudlets are regularly spaced, often arranged as ripples in the sky.
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cumulus 1. cumulus-a globular cloud. cumulus cloud. altocumulus, altocumulus cloud-a cumulus cloud at an intermediate altitude of 2 or 3 miles. cloud-a visible mass of water or ice particles suspended at a considerable altitude. thunderhead-a rounded projecting mass of a cumulus cloud with shining edges; often appears before a thunderstorm.
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Cumulonimbus cloud Cumulonimbus can form alone, in clusters, or along cold front squall lines. These clouds are capable of producing lightning and other dangerous severe weather, such as tornadoes.Cumulonimbus progress from overdeveloped cumulus congestus clouds and may further develop as part of a supercell.he cumulonimbus base may extend several miles across and occupy low to middle altitudes-formed at altitude from approximately 200 to 4,000 m (700 to 10,000 ft).
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Cumulonimbus cloud Cumulonimbus, from the Latin cumulus (heap) and nimbus (rainstorm, storm cloud), is a dense towering vertical cloud associated with thunderstorms and atmospheric instability, forming from water vapor carried by powerful upward air currents.
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- Photograph by: Holle. Altocumulus clouds are composed primarily of water droplets and are located between 6,500 and 20,000 feet (2,000 to 6,000 meters) above the ground. Photograph by: Holle. Altocumulus may appear as parallel bands (top photograph) or rounded masses (bottom photograph). Typically a portion of an altocumulus cloud is shaded, a characteristic which makes them distinguishable from the high-level cirrocumulus.