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With that in mind, let's dive into the four methods of cloud formation! Although every instance of cloud formation is different, chances are pretty high that one or more of these four processes are involved whenever you see clouds in the sky. Cumulus, stratus, cumulonimbus, and stratocumulus clouds that are below 6, 500 feet (1, 981 m). But, this is what you can expect from the various cloud heights: - Low-Level Clouds – These clouds form between the surface and 7, 000 feet (2, 000 m) above the ground. If the clouds are thin, the Sun might peek through, looking like a round disk. In summer they can form over mountains due to orographic lifting in combination with solar heating. They are made up of ice crystals and tend to be high, wispy clouds that show up first before a low-pressure area like a storm system in the middle latitudes or a tropical system like a hurricane. Cloud often seen in the summer festival. Since this air is very dry and since the air is very cold in the upper troposphere, the little moisture that remains in the air parcel transitions straight from water vapor to ice crystals in a process called deposition. Many displays of NLC are bright enough to photograph with the camera on your phone (if you hold it steady or mount it on a tripod), but you really need a digital SLR with a tripod and a wide-angle lens to take good NLC photographs.

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If the cloud is a cumulo-form but a rain cloud, it is termed cumulonimbus (more commonly called thunderclouds). Calvus – A tall cloud with a large, round, and puffy top. They often occur in the advance of a cold front. These falling ice crystals then leave behind a hole that we call a fallstreak. There are multiple sub-layers in the troposphere that we'll discuss in a bit. While these clouds are beautiful, however, researchers have recently discovered that they're actually contributing to the depletion of the ozone layer. For example, some air masses are warm and moist, such as those that originate over the subtropical waters of the Gulf of Mexico. When two air masses with different temperatures and moisture contents meet, their meeting point is called a front. Low, Medium, High Brings Different Cloud Types. These supplementary features and accessory clouds include: - Incus – Also known as an "anvil, " incus are associated with mature cumulonimbus clouds. Cirrostratus form as a large parcel of air rises very slowly and uniformly into the upper atmosphere.

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Depending on the thickness of the cloud, stratocumulus will have light to dark gray hues. Commonly called nacreous clouds or mother of pearl clouds, these clouds form in the stratosphere from about 6 to 15 miles (10 to 25 km) above the Earth's surface. Think of a cloudy, dreary day — a stratus cloud is likely looming above.

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The boundary between the air masses begins to ripple, eventually forming larger waves. Some of the best cloud pictures involve cirrostratus clouds because the ice crystals beautifully refract light from the sun or moon producing a dazzling halo effect. Altostratus Opacus – Seen on wet days, this is a gloomy species that, once it descends, transforms into the rain-bearing nimbostratus. These cloudlets are mostly made up of ice crystals and they often look like a fish's scaly skin when grouped together. Cumulus clouds are defined by their puffy, cotton candy-esque shape, so they're what most people are thinking of when they picture a fluffy cloud. The types of clouds: everything you need to know. The name "cumulus" actually comes from the Latin word of the same spelling that roughly translates to "heaps. " Found as stratus, cirrostratus, stratocumlus, and altostratus. In general, the air can hold more water vapor when it is warmer. They do not usually produce precipitation on their own, but they can form virga (more on this in a bit). Their appearance can change quite rapidly, and they can fade from view as swiftly as they appear.

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These varieties are somewhat similar to a subspecies when classifying animals and plants. Having said that, a pair of binoculars is great to have handy because NLC often have very fine, intricate internal structure that isn't obvious to the naked eye. Identifying The 10 Types of Clouds: Pictures & Chart (+ 14 Seldom Ones. Some clouds are as high as a jet; others kiss mountaintops. These clouds are common in summer when air rises due to convection resulting from solar heating of the surface. 3 Stratocumulus (Sc). These clouds form when the air is stable downwind of the mountain, the wind flows over the mountain in a wave-like pattern, and lenticular clouds are often generated in the ascending air over a mountain. Sometimes, these clouds can form severe thunderstorms with damaging winds, lightning, hail and even tornadoes.

Clouds Often Seen In The Summer

These clouds tend to be light to dark grey in color and they're often to blame when the sky is looking grey and dreary. For example, imagine a large mountain chain like the Rocky Mountains in the western United States. Clouds often seen in the summer. This is similar to how sundogs are made, but the halo is a full circle instead of just two sides. Most cirrus form ahead of a warm front, so they often indicate that changing weather is en route to your location.

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Although cloud spotting is a worthy activity in its own right, understanding how clouds form can help you better understand how to use clouds to track changes in the weather while you're outside. They are made of liquid water, but they don't often produce rain. These night-shining clouds, are only seen in the mid-summer months from higher latitudes in both the northern and southern hemispheres. Cloud often seen in the summer crossword. Altocumulus occur frequently and are common in many places of the world. According to the National Weather Service, a funnel cloud can be considered a tornado if it either touches the surface of the Earth or if it has a cloud of debris below it. Cirrus clouds light up long before other clouds and fade out much later.

Cirrus: Thin, feather-like, wispy clouds which are strands of ice crystals. These are low, puffy, grayish or white clouds that appear in patches with blue sky in between. Cumulus humilis – These cumulus clouds are wider than they are tall. Stratocumulus stratiformis – This is the most common type of cloud all across the globe. Once we move into the highest level of the troposphere, there are three main types of clouds that you ought to look out for. First up on our list are our low-level clouds, which are mostly found between the surface of the Earth and 7, 000 feet (2, 000 m) above the ground. The condensation level is the height at which the dew point is reached, and clouds start to form. When you look up at the sky, you may not realize that there's a lot more to our atmosphere than meets the eye. You may also see them out in front of cold fronts, which means that cooler weather is coming. These clouds are only found in the genus cumulonimbus. There are four species of cloud underneath the altocumulus genus: altocumulus lenticularis (stationary lens-shaped clouds that are often mistaken for UFOs) altocumulus castellanus (altocumulus with tower-like sproutings that billow upwards) altocumulus stratiformis (altocumulus in sheets or relatively flat patches) altocumulus floccus (altocumulus with scattered tufts and fringy lower parts) The abbreviation for altocumulus clouds is (Ac). Besides the filament appearance, cirrus clouds stand out among other types of clouds because they're often colored in bright yellow or red before sunrise and at sunset, respectively.

Cirrus clouds usually form when the weather is nice. The lighter warm air is forced to rise over the cold air mass, leading to cloud formation. They can grow to more than 7 miles (12 kilometers) tall.

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