Convective cloud gives showers, stratus gives steady precipitation.
The nimbostratus cloud is known to produce drizzle as it is a thick, dark cloud that brings steady and light precipitation. Drizzle is characterized by small water droplets that fall slowly and persistently from a cloud layer.
Light or moderate and steady precipitation is most often associated with nimbostratus clouds. These low-level, thick clouds are capable of producing prolonged and continuous precipitation due to their extensive coverage and stable structure.
Nimbostratus clouds are typically associated with steady rain that can last for an extended period of time. These clouds are thick, grey clouds that cover the sky and usually bring widespread precipitation.
The type of cloud one them self would see is a huge gray cloud
A warm front typically brings light steady rain or snow. As the warm air mass rises over the colder air ahead of it, the moisture condenses and forms precipitation. This precipitation is usually more prolonged and consistent compared to the heavy and intense rainfall associated with a cold front.
When the prefix "nimbo" is attached to another cloud type, it indicates that the cloud is producing precipitation. For example, nimbostratus clouds typically bring steady, widespread precipitation.
Steady rain is typically caused by a prolonged weather system, such as a low-pressure system or a frontal boundary, that brings moisture-laden air and sustained precipitation over an area for an extended period of time. This can result in a consistent and continuous rainfall.
The nimbostratus cloud is a somewhat shapeless, widespread, low-sitting cloud which broadly distributes precipitation. The nimbostratus cloud is usually an indication of steady, consistent rainfall.
The nimbostratus cloud is known to produce drizzle as it is a thick, dark cloud that brings steady and light precipitation. Drizzle is characterized by small water droplets that fall slowly and persistently from a cloud layer.
Light or moderate and steady precipitation is most often associated with nimbostratus clouds. These low-level, thick clouds are capable of producing prolonged and continuous precipitation due to their extensive coverage and stable structure.
A rain cloud is usually a "nimbus" cloud such as the nimbostratus and cumulonimbus (thunderstorm) clouds.
The type of cloud that produces precipitation is called a "nimbostratus" cloud. These clouds are thick, dark, and typically cover the sky, leading to steady, continuous rain or snow. Another type is "cumulonimbus," which can produce heavy rain, thunderstorms, and even severe weather like tornadoes. Both types are crucial for the water cycle and weather patterns.
Nimbus is the Latin word for cloud. In modern meteorology, it is used as a prefix or suffix on the names of particular types of clouds to indicate a cloud that is precipitating (rain, snow, hail, etc.). Thus a cumulonimbusis a cumulus cloud that is releasing precipitation and a nimbostratus is a status cloud releasing precipitation.
Any cloud, including clumlus.
Nimbostratus
cirrus
Nimbostratus clouds are typically associated with steady rain that can last for an extended period of time. These clouds are thick, grey clouds that cover the sky and usually bring widespread precipitation.