It condenses and becomes liquid water.
This description represents the process of condensation in the water cycle. Water vapor in the air cools and condenses to form clouds when it is mixed with cooler air, ultimately leading to precipitation.
Condensation occurs when water vapor, a gas, cools and transforms into liquid water droplets. This process commonly happens as warm, moist air rises and cools, leading to the formation of clouds or dew.
When warm air cools, water vapor in the air can condense into liquid water droplets or ice crystals, resulting in the formation of clouds or fog. This process is called condensation.
Water vapor in the air condenses when it cools below its dew point, which is the temperature at which the air becomes saturated with moisture. This can happen when warm air cools down, such as at night, or when moist air comes into contact with a cooler surface.
This process is called condensation. It happens when the temperature of water vapor decreases, causing the vapor to lose energy and transition into liquid form. Condensation is commonly observed when warm air cools down, such as when moisture in the air collects on a cold surface.
When air cools, it can no longer hold as much water vapor, so some of the water vapor might condense into liquid water droplets. This can lead to the formation of clouds or fog.
it condenses on the ground to make dew
Water vapor is called "condensation" when it cools and changes from a gas to a liquid.
air.
It condenses and it becomes liquid
Water vapor turns to water droplets causing it to rain.
Condensation occurs when water vapor in the air cools and turns back into liquid water. This typically happens when warm air comes into contact with a cooler surface, causing the air to cool down and its water vapor to condense into droplets.
This description represents the process of condensation in the water cycle. Water vapor in the air cools and condenses to form clouds when it is mixed with cooler air, ultimately leading to precipitation.
Condensation occurs when water vapor, a gas, cools and transforms into liquid water droplets. This process commonly happens as warm, moist air rises and cools, leading to the formation of clouds or dew.
When warm air cools, water vapor in the air can condense into liquid water droplets or ice crystals, resulting in the formation of clouds or fog. This process is called condensation.
Water vapor in the air condenses when it cools below its dew point, which is the temperature at which the air becomes saturated with moisture. This can happen when warm air cools down, such as at night, or when moist air comes into contact with a cooler surface.
No, condensation happens when warm air cools down, causing the water vapor in the air to reach its dew point and change into liquid moisture. As the air cools, its capacity to hold water decreases, leading to the formation of water droplets on surfaces.