what are stratus clouds
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Stratus clouds â A blanket of cloud â Weather science If you see stratus clouds, that's the time to get inside and stay there. Stratus clouds mean rain if it is warm and snow if it is cold. They look like a huge gray blanket that hangs low in the sky. Sometimes stratus clouds are on the ground or very near the ground, and then we call them fog. Usually stratus clouds and fog form when it has been cold out and then warmer, wet air blows in. As the warm air flows over the cold ground or over the cold air near the ground, the water vapor in the warm air condenses into drops of water that make a cloud.
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- Stratus (St). Found at very low levels (less than 2000 meters, or 6500 feet), stratus clouds are thick, large, heavy-looking gray clouds that dominate the sky. Precipitation normally does not occur with this cloud, although drizzle or mist may be observed.
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- Found at very low levels (less than 2000 meters, or 6500 feet), stratus clouds are thick, large, heavy-looking gray clouds that dominate the sky. Precipitation normally does not occur with this cloud, although drizzle or mist may be observed. This type of cloud resembles fog, and occasionally when fog lifts, it will form a stratus cloud deck. Latin Derivative: stratus - layer http://www.msstate.edu: Nimbostratus (Ns) Nimbostratus clouds are also found below 2000 meters. They are usually a darker color of gray than stratus clouds because of their high moisture content - precipitation usually occurs with this cloud type. The base of this cloud can be difficult to identify and it may stretch high into the atmosphere.
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High Clouds â Definition High Clouds. A term used to signify cirriform clouds that are composed of ice crystals and generally have bases above 20,000 feet. The main types of high clouds are cirrus, cirrocumulus, and cirrostratus. This altitude applies to the temperate zone. In the polar regions, these clouds may be found at lower altitudes. In the tropics, the defining altitudes for cloud types are generally higher. Cirriform. Clouds composed of small particles, mostly ice crystals.
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Cloud Classification Altostratus clouds are strato type clouds (see below) that possess a flat and uniform type texture in the mid levels. They frequently indicate the approach of a warm front and may thicken and lower into stratus, then nimbostratus resulting in rain or snow.
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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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Cloud When a low stratiform cloud contacts the ground, it is called fog if the prevailing surface visibility is less than 1 kilometer, although radiation and advection types of fog tend to form in clear air rather than from stratus layers.
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Stratus cloud This can also occur on nimbostratus clouds (stratus nimbostratogenitus) and on cumulonimbus clouds (stratus cumulonimbogenitus). Stratus fractus clouds can also form under the base of precipitation-bearing clouds and are classified as pannus clouds.
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Types Of Water Stratus clouds are among the low-lying clouds. They are gray clouds that cover the entire sky and can be the result of very thick fog lifting in the morning.Nimbostratus clouds are dark gray clouds that produce falling rain or snow.Cumulus and cumulonimbus clouds are both known as vertical clouds.
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- They are usually a darker color of gray than stratus clouds because of their high moisture content-precipitation usually occurs with this cloud type. The base of this cloud can be difficult to identify and it may stretch high into the atmosphere.Latin Derivatives: nimbus - violent rain and stratus - layer.
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List of cloud types 1 Cumulonimbus (WMO genus) – heaped towering rain-bearing clouds that stretch to the upper levels of the troposphere. 2  Cumulonimbus calvus (WMO genus and species) – cumulonimbus with round tops like cumulus congestus.
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Cloud Classification The three main types of high clouds are cirrus, cirrostratus, and cirrocumulus. Cirrus clouds are wispy, feathery, and composed entirely of ice crystals. They often are the first sign of an approaching warm front or upper-level jet streak. Unlike cirrus, cirrostratus clouds form more of a widespread, veil-like layer (similar to what stratus clouds do in low levels).
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strato- strato-. 1. a combining form representing stratus, (stratocumulus) or specialized as a combining form of stratosphere (stratovision). strato-. 1.
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What Are Clouds? High Clouds. Cirrus (Ci): The ice-crystal cloud is a feathery white cloud that is the highest in the sky. It has a wispy looking tail that streaks across the sky and is called a fallstreak. Cirrus Clouds. Cirrostratus (Cs): A milky sheet of ice-crystal cloud that spreads across the sky.
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Clouds Clouds are classified into four basic categories, depending largely on the height of their bases above the ground. High-level clouds, called cirrus clouds, can reach heights of 20,000 feet (6,000 meters) and are typically thin. They do not produce rain and often indicate fair weather. They are usually made up of ice.
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- Fog- Fog is a cloud that has the base on the earth's surface. Fractus- Fractus are also known as scud and cloud tags. They are isolated low level stratus clouds that can often be seen around the base of thunderstorms. They often look unorganized and flow with the low level wind.
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- Marine Layer clouds that impact California are low altitude stratus clouds that form over the adjacent ocean waters. Once formed, they may be advected by the wind over land areas. Stratus type clouds are sheet like clouds with close to horizontally uniform base and top.
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How Do Stratus Clouds Form? These water droplets are what the stratus cloud is comprised of. Cirrostratus and altostratus clouds form at altitudes above 6,000 feet in elevation, while nimbostratus and cumulostratus clouds form below 6,000 feet.
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Altocumulus and altostratus clouds usually bring which of the following types of weather? hot, windy conditions heavy snow or rain light snow or rain sunny skies Usually alto-cumulus and alto-stratus are clouds that have been slowly lifted by the very slack slope of a warm front. The normal progression of this type of weather is to see the ceiling to go down, drizzle to happen, the wind to increase and dark nimbostratus and cumulonimbus full of rain or snow. Report.
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Stratus Clouds Stratus clouds may also form from the cooling of moist air. When fog is warmed by the sun, it will rise and eventually condense forming stratus clouds. This is usually seen over lakes.
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- The last variation on stratus clouds is the stratocumulus cloud. Occurring below 2000 meters, these clouds resemble little rows of cotton balls. The coloring of these clouds can vary from gray to white depending on the sunlight angle.
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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. 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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