It turns out that there are many distinct forms of clouds. In the non-mountainous parts of the southwest United States during the summer, the base of these convective clouds will be well into the mid-level cloud range. They can look like pieces of floating cotton. Their appearance can change quite rapidly, and they can fade from view as swiftly as they appear. Here's how it works. He called it Undulatus asperatus, an odd cloud formation with a distinct undulating and rolling motion. These tend to form at less than 6, 500 feet (1.
The puffy, mound-shaped clouds that you see on sunny days, cumulus clouds are normally white or light grey. Stratus: Thin, gray-white, sheetlike clouds with low bases covering the whole sky. Bellwethers of Bad Weather Altocumulus clouds that appear on a clear humid morning can indicate the development of thunderstorms later in the day. Near the ground, Cumulonimbus are well defined, but higher up they start to look wispy at the edges. What Are The Big Fluffy Clouds Called? Next time take notice if you see more of these clouds during the afternoon, the warmest part of the day. They appear with a beautiful shimmering glow, after the Sun has set and the sky has darkened. These clouds look surprisingly similar to ocean waves, which is why they're so amazing to look at. Cirrocumulus: Thin clouds that appear as small "cotton patches. These clouds are relatively simple to identify because they look like strands of thin, white hair.
Their delicate, feathery shape comes from wind currents which twist and spread the ice crystals into strands. This can make them look quite dramatic, especially when the dark skies of a thunderstorm trail closely behind. Rather, they do not produce lightning on their own and they are generally responsible only for rain, snow, and other types of precipitation. These clouds are only found in the genus cumulonimbus. They tend to form as a result of a very strong updraft and lots of moisture in the atmosphere. The author of a new study explains how adding light could dramatically increase the electrical conductivity of bacteria-grown nanowires. Some of the more common optical effects that you might see with altostratus include cloud iridescence and coronas, so keep your eyes peeled if these clouds are in the sky. Cirrus castellanus – More vertically developed and have a turret-like summit. Sometimes considered to be the "king of clouds, " the cumulonimbus is a truly spectacular atmospheric phenomenon. When arcus clouds move overhead, it can look like they're literally rolling over the ground below. The Sub-Tropical Jet Stream runs roughly between the Temperate Regions and the Tropical Regions. Cirrostratus: Since it is a stratus cloud, even high in the sky it resembles an almost uniform layer. As outlined earlier, a nimbostratus cloud can form from other types of clouds, like a descending altostratus.
Over the central United States, they also form from outflow of severe thunderstorms. Needless to say, if you see a funnel cloud on the horizon, please take shelter. Cite this Article Format mla apa chicago Your Citation Oblack, Rachelle. Cumulus congestus tilt if the wind speed increases with altitude. Smooth, lens-shaped Lenticular clouds form as air is blown up and over a mountain range. Supplementary Features & Accessory Clouds. Altocumulus stratiformis – Looks like a bunch of flat-bottomed puffy clouds packed tightly together but separated by small streaks. Altocumulus is roughly as wide as your thumb at arm's length. Industrial pollution may also produce the clouds. Many have unique shapes or odd formation patterns that make them difficult to categorize elsewhere. Most of the clouds in the middle atmosphere tend to be what are called altocumulus clouds.
Therefore, just like air that's heated at the Earth's surface, air that's forced upward through a region of low pressure will rise, cool, and condense into a cloud. But more on that in the next section. Floccus – Clouds that have small, puffy tufts and wispy tails. These clouds are known for their large, arch-shaped formation, which makes them look particularly foreboding ahead of an advancing thunderstorm.
Noctilucent clouds are the highest type of cloud in Earth's atmosphere. These clouds are typically classified as low-level clouds, but they actually form mostly in the mid-level of the troposphere. Mammatus cloud derive their name from their pouch-like appearance. What Is The Most Dangerous Cloud? Cirrus form very high in the atmosphere. These virga represent precipitation that's falling from a cloud but that evaporates into the atmosphere before it ever hits the ground. Once you understand how clouds form through surface heating, you're in a good position to understand how cloud formation through low pressure works, too. 9 km) on hot days when warm, wet air rises very high into the sky. Altostratus species. Cumulonimbus clouds form in unstable, moist atmospheres and are common in spring and summer. These rainbow colors are the result of an optical phenomenon called cloud iridescence, which is quite the sight to see. These ice crystals then bind to water droplets in the cloud layer that freeze, grow, and then precipitate out of the cloud layer before evaporating lower down in the troposphere. Cirrostratus fibratus – It looks a lot like cirrus only with more consistency.
However, there are some subtypes of stratus clouds, such as the stratus fractus, that form in irregular, broken shapes. All well and good, but let's dig into the clouds in a little more detail, shall we? Stratocumulus lenticularis – The rarest variety of stratocumulus, these are often spotted in hilly locations which produce atmospheric waves. They are also sometimes referred to as mesospheric clouds, due to their location above us. Many of these may already be familiar to you, but it's important that we're all on the same page before we start talking about cloud formation. 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 first type of cloud classification system that you might see is one where clouds are organized based on their typical altitude in the sky. This kind of fog is called "radiation fog" because it is caused by radiational cooling, which is when heat from the ground cools the air.
The lighter warm air is forced to rise over the cold air mass, leading to cloud formation. Found only in the mesosphere at an elevation of 31 to 53 miles (50 to 85 km) above the Earth's surface, noctilucent clouds are the world's highest clouds. There are two main ways to reach a point of saturation. Clouds may also form in contact with the ground surface, too — it's just called fog, ice fog, or mist.
As it sinks, it warms and the cloud evaporates. They often produce precipitation that is usually light to moderate. This occurs because the air can only hold a certain amount of water vapor at a certain temperature. Stratus may also originate when moist, cold air is advected at low altitudes over a region. Supplementary features and accessory clouds, however, are not necessarily an integral part of the cloud itself. The diagram below provides a quick overview of the most common types of clouds based on altitude. If the sun appears through these clouds, it has a "watery" appearance.
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