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Stratus clouds are commonly associated with warm fronts. As the warm air mass rises over a cooler air mass, it cools and condenses to form stratus clouds, often resulting in overcast and rainy conditions.
Generally speaking, both stratiform and convective clouds will produce precipitation. So stratus cloud ("scud") and stratocumulus will produce drizzle, cumulus and/or cumulonimbus will produce showers of rain, snow or hail, while altostratus and nimbostratus will produce rain or snow. The middle level cloud altocumulus castellanus will produce light showers. Cirrus is composed of ice crystals and while virga (rain falling but evaporating) can sometimes be seen, high level cloud rarely produces precipitation. Bear in mind that the low, middle and high cloud etages vary in height with latitude so cirrus may be reported over polar regions at 10,000 ft, so it's possible that precipitation may fall from cirrus over high latitude regions.
AnswerStratus clouds begin when a warm, moist airmass is forced over a cold air mass, essentially a cold front. This forms the cloud. Eventually, it starts precipitating, which drops all the moisture onto the earth. Then, there's no more cloud afterwards.
The three major clouds are cumulus, stratus, and cirrus. Cumulus are fluffy with flat bottoms. Stratus are formed in layers. Cirrus are 'feathery' clouds. Whenever the word alto is in front of the cloud name (for example, altostrautus), this means the cloud is somewhere in between 2000 and 7000 feet in the atmosphere. Whenever the word nimbo is in front of the cloud name (for example nimbocumulus), it means the cloud is a dark rain cloud.
Cirrus clouds form above 6000 meters. They are thin, wispy clouds that are composed of ice crystals and indicate fair weather or the approach of a warm front. Stratus clouds are typically lower in altitude and are more uniform in appearance compared to cirrus clouds.
Stratus clouds are commonly associated with warm fronts. As the warm air mass rises over a cooler air mass, it cools and condenses to form stratus clouds, often resulting in overcast and rainy conditions.
Stratus clouds and drizzly rain :)
Stratus clouds and drizzly rain :)
Generally speaking, both stratiform and convective clouds will produce precipitation. So stratus cloud ("scud") and stratocumulus will produce drizzle, cumulus and/or cumulonimbus will produce showers of rain, snow or hail, while altostratus and nimbostratus will produce rain or snow. The middle level cloud altocumulus castellanus will produce light showers. Cirrus is composed of ice crystals and while virga (rain falling but evaporating) can sometimes be seen, high level cloud rarely produces precipitation. Bear in mind that the low, middle and high cloud etages vary in height with latitude so cirrus may be reported over polar regions at 10,000 ft, so it's possible that precipitation may fall from cirrus over high latitude regions.
precipitation over a large area with stratus cloudsstormy clouds
AnswerStratus clouds begin when a warm, moist airmass is forced over a cold air mass, essentially a cold front. This forms the cloud. Eventually, it starts precipitating, which drops all the moisture onto the earth. Then, there's no more cloud afterwards.
The three major clouds are cumulus, stratus, and cirrus. Cumulus are fluffy with flat bottoms. Stratus are formed in layers. Cirrus are 'feathery' clouds. Whenever the word alto is in front of the cloud name (for example, altostrautus), this means the cloud is somewhere in between 2000 and 7000 feet in the atmosphere. Whenever the word nimbo is in front of the cloud name (for example nimbocumulus), it means the cloud is a dark rain cloud.
The answer for this question would be: stratus clouds and drizzly rain
Cirrus clouds form above 6000 meters. They are thin, wispy clouds that are composed of ice crystals and indicate fair weather or the approach of a warm front. Stratus clouds are typically lower in altitude and are more uniform in appearance compared to cirrus clouds.
stratus
air and water
Stratiform clouds, such as stratus or nimbostratus clouds, form when warm moist air rises over a layer of cool air. As the warm air cools and condenses, it creates a blanket-like cloud layer that can result in overcast or rainy conditions.