water
In a warm occlusion, clouds and precipitation would form at the boundary where the warm air rises above the cooler air. In a cold occlusion, clouds and precipitation would form along the front where the advancing cold air lifts the warm air. In a stationary occlusion, clouds and precipitation would occur at the boundary between the cool and cold air masses that are not actively moving.
Cumulonimbus clouds are responsible for producing thunderstorms. These towering clouds are formed by strong updrafts of warm, moist air that lead to the development of thunder, lightning, and heavy precipitation.
condense into tiny water droplets. This process is known as condensation and is responsible for the formation of clouds and other forms of precipitation.
Nimbus clouds are the type of clouds that are typically associated with rain. These clouds are characterized by their dark, thick appearance and are responsible for producing precipitation in the form of rain.
Droplets that become too heavy to remain suspended in the air fall out of the clouds as precipitation, such as rain, snow, sleet, or hail.
Water vapor typically remains in the air for a few days before it condenses and forms clouds or precipitation.
Clouds responsible for precipitation are typically nimbostratus clouds, which are thick, dark clouds that cover the sky and bring steady rainfall. Cumulonimbus clouds, which are tall and dense, can also produce heavy rain showers or thunderstorms. Both types of clouds contain water droplets that eventually coalesce and fall as precipitation when they become too heavy to remain suspended in the atmosphere.
a mid- precipitation and a few rain clouds and a high humidity.
Cold air and warm air coming together in a front, or water evaporating, condensing into clouds, and then the clouds fall down as rain.
The warm air rises and cools, causing condensation of water vapor which leads to the formation of clouds. Eventually, the water droplets in the clouds combine and fall as precipitation, such as rain or thunderstorms.
Precipitation
Convection