stratiform clouds definition
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Stratus cloud (Redirected from Stratiform). Stratus clouds are low-level cloud characterized by horizontal layering with a uniform base, as opposed to convective or cumuliform clouds that are formed by rising thermals.
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Cirrostratus cloud Cirrostratus cloud. Cirrostratus /ˌsɪroʊˈstrɑːtəs/ is a high-level, very thin, generally uniform stratiform genus-type of cloud, composed of ice-crystals. It is difficult to detect and is capable of forming halos when the cloud takes the form of thin cirrostratus nebulosus.
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- Lenticular cloud. Lenticular clouds (Altocumulus lenticularis) are stationary lens-shaped clouds that form in the troposphere, normally in perpendicular alignment to the wind direction.
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Types of Clouds Cirrostratus 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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What are the major cloud types? What type of weather is associated with each type? Cumulonimbus clouds are the tallest clouds and can gorw to be 20,000ft and have an anvil top. Cumulus congestus is the developing stage for cumulonimbus. Cumulonimbus brings heavy precipitation. Most cumulus clouds are known as fair weather cumulus clouds in blue skies. Stratiform clouds streach across the sky in layers.
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- 2. : an accumulation of granular ice tufts on the windward sides of exposed objects that is formed from supercooled fog or cloud and built out directly against the wind.. : an accumulation of granular ice tufts on the windward sides of exposed objects that is formed from supercooled fog or cloud and built out directly against the wind.
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- Snow falls from nimbostratus clouds. Nimbostratus clouds are grey, thick, low-level cpouds that cover the entire sky. These kinds of clouds are associated with prolonged weather, mainly rain or snow. Fun fact : The root word for nimbus, 'nimbo', is Latin for rain or precipitation and the root word for stratus, 'strato', is Latin for layer.
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Definitions &Translations Wiktionary(0.00 / 0 votes)Rate this definition: polar stratospheric cloud(Noun) A relatively rare type of clouds that occurs high in the stratosphere; polar stratospheric clouds often resemble mother-of-pearl as they shine in vivid colours, known as irisation.
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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.
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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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Meet clouds by name HIGH. Clouds forming in high altitudes are called cirrus, cirrostratus, and cirrocumulus. It is so cold in the upper atmosphere that high altitude clouds contain ice crystals instead of water particles. CIRRUS clouds form when the wind blows these ice crystals into wispy streaks that look like thin horse tails.
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- HIGH LEVEL CLOUDS. The type of clouds most often found in the high level etage are cirrus, cirrocumulus and cirrostratus. These clouds are composed primarily of ice crystals and usually present a bright white, or mostly white appearance except near sunrise or sunset.
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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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Cirrus cloud Cirrus (cloud classification symbol: Ci) is a genus of atmospheric cloud generally characterized by thin, wispy strands, giving the type its name from the Latin word cirrus, meaning a ringlet or curling lock of hair.[1][2] This cloud can form at any altitude between 16,500 ft (5.0 km) and 45,000 ft (14 km) above sea level.
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Stratocumulus cloud This often does not apply when stratocumulus is of a broken, fractus form, when it may appear as small as altocumulus. Stratocumulus is also often, though not always, darker in colour than altocumulus. Stratocumulus clouds are the main type of cloud that can produce crepuscular rays.
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What are Stratus Clouds? Stratus clouds are similar to altostratus clouds, but form at a lower altitude and are identified by their fog-like appearance, lacking the distinguishing features of most clouds. Stratus clouds are wider than most clouds, and their base has a smooth, uniform look which is lighter in color than a nimbostratus cloud.
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- Cumulus 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. Here are some examples of cumulus clouds: Cumulonimbus clouds are thunderstorm clouds that form if cumulus congestus clouds continue to grow vertically.
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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 Couds form a greyish veil over the sun or moon.
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- Cirrus clouds are thin, white clouds that have a wispy, feathery  appearance. They form at heights of 25,000 feet or more. They are  composed of tiny ice crystals, and are a…ssociated with fair or  pleasant weather. They have a hair-like appearance, and the  curled-up ends are very common features.
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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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Types of Clouds Cumulonimbus clouds are thunderstorm clouds. High winds can flatten the top of the cloud into an anvil-like shape. Cumulonimbus clouds are associated with heavy rain, snow, hail, lightning and even tornadoes. The anvil usually points in the direction the storm is moving.igh winds can flatten the top of the cloud into an anvil-like shape. Cumulonimbus clouds are associated with heavy rain, snow, hail, lightning and even tornadoes. The anvil usually points in the direction the storm is moving.
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Weather The temperature of the collecting surface is at or below the dewpoint of the adjacent air and the dewpoint is below freezing. Stratiform clouds. A pilot can expect a wind-shear zone in a temperature inversion whenever the windspeed at 2,000 to 4,000 feet above the surface is at least.
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Cloud Polar stratospheric clouds show little variation in structure and are limited to a single very high range of altitude of about 15,000–25,000 m (49,200–82,000 ft), so they are not classified into étages, genus types, species, or varieties in the manner of tropospheric 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.