what clouds are with warm front?
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Warm fronts produce clouds when warm air replaces cold air by sliding above it. Many different cloud types can be created in this way: altocumulus, altostratus, cirrocumulus, cirrostratus, cirrus, cumulonimbus (and associated mammatus clouds), nimbostratus, stratus, and stratocumulus.
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A cold weather front is defined as the changeover region where a cold air mass is replacing a warmer air mass. Cold weather fronts usually move from northwest to southeast. Warm fronts usually move from southwest to northeast and the air behind a warm front is warmer and moister than the air ahead of it. ...
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Cumulonimbus clouds are born through convection, often growing from small cumulus clouds over a hot surface. ... They can also form along cold fronts as a result of forced convection, where milder air is forced to rise over the incoming cold air.
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['Sunrise. Sunset. Clear. Partly cloudy. Hot. Dust. Haze. Smoke. Fog.', 'Windy. Cloudy. Thunderstorms. Showers. Heavy showers. Drizzle. Hail/Mixed rain. Hurricane. Tornado.', 'Snow. Scattered snow. Heavy snow/Sleet. Blowing snow. Frigid temps. Cloudy. Clear.']
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A stationary front is a boundary between cold and warm air masses that aren't moving. These are more common in the Summer time when weather patterns don't move as much. You can spot them on a weather map because they look like a cold front and a warm front had a really bad head on collision.
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How do cumulonimbus clouds form? Cumulonimbus clouds are born through convection, often growing from small cumulus clouds over a hot surface. ... They can also form along cold fronts as a result of forced convection, where milder air is forced to rise over the incoming cold air.
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High-level clouds: The three main types of high clouds are cirrus, cirrostratus, and cirrocumulus. Cirrus clouds are wispy, feathery, and composed entirely of ice crystals. ... 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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As it is the highest form of cloud I'd suggest that the noctilucent clouds are the very least likely ones to produce precipitation that reaches the ground. These clouds are found way up around 80 kilometres above the surface of the earth.
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Clouds are categorized according to two main characteristics: height in the atmosphere (low, middle, or high) and shape (nimbus, stratus, cumulus, or cirrus). Cloud types are named using combinations of height and shape characteristics and provide information about how clouds form and behave.
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Basically, a weather front represents a boundary between two different air masses, such as warm and cold air. If cold air is advancing into warm air, a cold front is present. On the other hand, if a cold air mass is retreating and warm air is advancing, a warm front exists.
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['Breeze. The formation of sea and land breeze form the classic examples of convection. ... ', 'Boiling Water. Convection comes into play while boiling water. ... ', 'Blood Circulation in Warm-Blooded Mammals. ... ', 'Air-Conditioner. ... ', 'Radiator. ... ', 'Refrigerator. ... ', 'Hot Air Popper. ... ', 'Hot Air Balloon.']
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Cumulus clouds form in areas where the ground is very warm. The warm air on the ground speeds the evaporation of surface water. That moisture gets pulled up into the atmosphere by an uplift. The warm air carrying moisture enters cooler temperatures higher in the atmosphere.
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["Troposphere. The troposphere starts at the Earth's surface and extends 8 to 14.5 kilometers high (5 to 9 miles). ... ", 'Stratosphere. The stratosphere starts just above the troposphere and extends to 50 kilometers (31 miles) high. ... ', 'Mesosphere. ... ', 'Thermosphere. ... ', 'Ionosphere. ... ', 'Exosphere. ... ', 'Credit: NASA/Goddard.']
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The type of front depends on both the direction in which the air mass is moving and the characteristics of the air mass. There are four types of fronts that will be described below: cold front, warm front, stationary front, and occluded front.
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A spectacular, swirling cloud forms above a mountain range in New Zealand - a country known by Maoris as The Land of the Long White Cloud. The formation, known as a lenticular cloud, was captured at sunset by Chris Picking in the foothills of the Tararua Range in the southern part of New Zealand's North Island.
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Maritime Tropical Air Masses: warm temperatures and rich in moisture. Maritime tropical air masses originate over the warm waters of the tropics and Gulf of Mexico, where heat and moisture are transferred to the overlying air from the waters below.
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At the upper reaches of the troposphere you'll find high clouds, which, depending on geographic location, occur between roughly 10,000 and 60,000 feet. Below that is the home of mid-level clouds, which generally occur between 6,000 and 25,000 feet.