Clouds occur when moist air is cooled. This usually a fall in barometric pressure, or expansion in our atmosphere. There are other factors at work, however, one of them is called adiabatic heating and cooling. When a volume of air is compressed, its temperature rises, and when it is decompressed, or expanded, then it cools. In the case of cloud formation, it is the drop in temperature by adiabatic cooling, and the content of moisture in the air, that make the difference in how clouds are formed.
Cumulonimbus, or thunderstorm, clouds form from rising moist air.
Cumulus clouds is an resault of updraft of warm,moist air in tall clouds.
Clouds form when warm moist air rises, cools and condenses.
Moist air is cooled below its condensation point.
Generally not. Clouds generally form when moist air is cooled until some of the moisture in it condenses into droplets or freezes into ice crystals. This cooling can occur as a result of contact with cooler air, night time cooling, or cooling due to decompression.
Cumulonimbus, or thunderstorm, clouds form from rising moist air.
Moist air. Clouds are condensation from water vapor.
Cumulus clouds is an resault of updraft of warm,moist air in tall clouds.
Moist = clouds = heat retention Desert = no clouds = heat loss = cooler
Clouds moist air.
Orographic Clouds
Clouds form when warm moist air rises, cools and condenses.
Many
Warm, moist air.
Moist air is cooled below its condensation point.
Generally not. Clouds generally form when moist air is cooled until some of the moisture in it condenses into droplets or freezes into ice crystals. This cooling can occur as a result of contact with cooler air, night time cooling, or cooling due to decompression.
cools and condenses