When warm, moist air rises, it cools as it expands in the upper atmosphere. As the air cools, the water vapor it contains condenses into tiny droplets, forming clouds. This process releases latent heat, which can further affect air movement and create wind. The resulting differences in air pressure and temperature drive the circulation of air, contributing to wind patterns.
Cooler. The cloud forms because the water vapor condenses by cooling down. Thunderstorms occur because a warm, moist air mass is cooled by an incoming cold air mass. When the moist air gets chilled, the water vapor condenses to form clouds, resulting in rain.
Water vapor forms clouds when it condenses in the atmosphere.
Clouds form in the sky when water vapor condenses into water droplets. This process occurs when warm, moist air rises and cools, causing the water vapor to condense around particles in the atmosphere, such as dust or pollen, forming clouds.
Clouds form in the sky when water vapor condenses into water droplets. This process occurs when warm, moist air rises, cools, and reaches its dew point, causing the water vapor to condense and form visible clouds.
Water vapor does not produce a waste product. When water vapor condenses, it forms liquid water.
Cooler. The cloud forms because the water vapor condenses by cooling down. Thunderstorms occur because a warm, moist air mass is cooled by an incoming cold air mass. When the moist air gets chilled, the water vapor condenses to form clouds, resulting in rain.
when water vapour is cooled it condenses and falls as rain
When warm air filled with water vapor cools off, the water vapor condenses into tiny water droplets or ice crystals. This condensation forms clouds and, if the cooling continues, precipitation such as rain, snow, or hail may occur.
When air is cooled, the gas that typically condenses first to form a liquid is water vapor. This process occurs at a specific temperature known as the dew point, where the air becomes saturated with moisture and water vapor condenses into liquid water droplets.
When water vapor is cooled, it loses energy and condenses back into liquid water. This process is called condensation.
Water vapor forms clouds when it condenses in the atmosphere.
Condensation.
When water vapor loses energy it "turns" into a liquid
When cooled, water vapor condenses into tiny water droplets due to a decrease in temperature, leading to the formation of clouds or fog. This process occurs when the air becomes saturated with water vapor, causing it to change from a gas to a liquid state.
evaporation
The water vapor condenses on striking the glass of drink. Hence they convert into water and it is felt moist outside.
Clouds form in the sky when water vapor condenses into water droplets. This process occurs when warm, moist air rises and cools, causing the water vapor to condense around particles in the atmosphere, such as dust or pollen, forming clouds.