cumulus-nimbus clouds or thick dark clouds
so basically cloud ♥
CLOUDS
When air rises in the atmosphere it decompresses and cools. This can cause moisture in the air to condense and form precipitation.
No, clouds form when warm, moist air rises and cools, causing water vapor to condense into water droplets or ice crystals. When air sinks, it typically becomes warmer and drier, which discourages cloud formation.
convection and subsidence
When warm moist air rises, it cools, causing the water vapor it contains to condense and form clouds. As the air continues to rise, this condensation can lead to precipitation such as rain, snow, or hail. This process is known as adiabatic cooling and is responsible for the formation of most weather phenomena.
Warm air rises in the atmosphere because it is less dense than cold air. As it rises, it cools and can form clouds and eventually trigger precipitation. This process is known as convection.
Objects that form as warm air rises and then cools are typically clouds. As warm, moist air ascends, it expands and cools, leading to condensation of water vapor into tiny droplets or ice crystals, depending on the temperature. This process creates various types of clouds, such as cumulus or stratus, which are visible formations in the atmosphere. Additionally, this cooling process can lead to the formation of precipitation, such as rain or snow.
Clouds form when warm, moist air rises and cools, causing the water vapor in the air to condense into water droplets or ice crystals around particles like dust or salt. These tiny droplets then collect together to form clouds.
Clouds form as warm air rises because as air rises, it expands and cools, which can cause the air to reach its dew point temperature where water vapor condenses into water droplets, forming clouds. At lower altitudes, the air is usually warmer and has not risen enough to cool and reach its dew point, so clouds do not form as easily.
One example is clouds forming as warm air rises, expands, and cools in the atmosphere. The cooling causes water vapor in the air to condense into tiny water droplets or ice crystals, creating visible cloud formations. This process is known as adiabatic cooling.
Warm air rises because it is less dense than cold air, creating an upward movement. As warm air rises, it cools down and becomes denser, then sinks back down. This cycle of warm air rising and cold air sinking creates convection currents.
Warm air expands and cools as it rises; the temperature decreases below dew point, so the water vapour changes phase from gas to liquid