do stratus clouds bring rain?
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Almost all rain is produced from low-level clouds. Stratus clouds produce steady rains, and cumulus clouds produce intense, stormy precipitation.
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Nimbostratus Clouds. Nimbostratus clouds are a type of low-level cloud, occurring below 6,000 feet. ... This low-intensity precipitation can last for several hours or several days. Because they form in conditions unfavorable to vertical development, nimbostratus clouds never produce heavy rains or thunderstorms.
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Most of the time this is because there is insufficient heating/lifting or moisture to cause deeper (taller) cloud development. These clouds are too thin to produce rain, lightning, or waterspouts.
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All in all, there are ten fundamental types of clouds. Often, you'll some places simply class clouds as cirrus, stratus, and cumulus because these clouds are the most common and representative for each altitude class. High-level clouds (5-13 km): cirrocumulus, cirrus, and cirrostratus.
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How do nimbostratus clouds form? Nimbostratus clouds form through the deepening and thickening of an altostratus cloud, often along warm or occluded fronts. These clouds extend through the lower and mid-layers of the troposphere bringing rain to the surface below.
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The foundation consists of 10 major cloud types. In addition to cirrus, stratus, cumulus, and nimbus clouds, there are cirrostratus, cirrocumulus, altostratus, altocumulus, stratocumulus, nimbostratus, and cumulonimbus clouds. The following table places these cloud types into the four major cloud groups.
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['High cloud - cirrus, cirrocumulus, cirrostratus.', 'Middle cloud - altostratus, altocumulus, nimbostratus.', 'Low cloud - stratus, stratocumulus.', 'Vertical - cumulus, cumulonimbus.']
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Rain and Hail: liquid and ice precipitation. Rain develops when growing cloud droplets become too heavy to remain in the cloud and as a result, fall toward the surface as rain. ... Hail is a large frozen raindrop produced by intense thunderstorms, where snow and rain can coexist in the central updraft.
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Pressure Changes Cause Weather Changes As air rises, it cools and water vapor within the air is unable to remain a gas. It forms tiny water droplets, making clouds in the sky. Remember to bring an umbrella with you on low pressure days because those clouds might cause precipitation.
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But why exactly does it rain so much in the Pacific Northwest? ... When moist winds blow inland with an approaching storm, the high terrain of the Cascade Range forces the moist air to rise into the atmosphere, enhancing the thick clouds and steady rainfall.
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Clouds Form in Different Ways As it rises, its pressure and temperature drop causing water vapor to condense. Eventually, enough moisture will condense out of the air to form a cloud. Several types of clouds form in this way including cumulus, cumulonimbus, mammatus, and stratocumulus clouds.
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Liquid water falling from the sky is of course most often called rain but how is this different from drizzle? It's down to the size of the droplets. If the water droplets are smaller than 0.5mm it's known as drizzle; 0.5mm or bigger and it becomes rain.
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Originally Answered: Are clouds part of the atmosphere? Yes clouds are part of the atmosphere. Clouds occur when air condenses due to colder temperatures found at higher altitudes and and turns into water vapour which we see as the many different type of clouds that we are familiar with.
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A cumulonimbus incus (Latin incus, "anvil") also known as an anvil cloud is a cumulonimbus cloud which has reached the level of stratospheric stability and has formed the characteristic flat, anvil-top shape. It signifies the thunderstorm in its mature stage, succeeding the cumulonimbus calvus stage.
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Stratus clouds hang low in the sky as a flat, featureless, uniform layer of grayish cloud. They resemble fog that hugs the horizon (instead of the ground).
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When the air hits the top of the atmosphere, it spreads north and south toward the poles. It does not sink back down until it is over the subtropics, but as it does, the air warms and dries out, creating deserts and other areas that are nearly devoid of rain.
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The air cools as it rises. Water vapor condenses and forms cumulus clouds. When condensation occurs, heat (latent heat/energy ) is released and helps the thunderstorm grow. At some point, condensation high in the cloud (now in the form of water droplets and ice) falls to the ground as rain.