Water vapor can remain in the air for varying amounts of time before it condenses into liquid form, depending on factors such as temperature, humidity, and air pressure. Generally, water vapor can stay in the air for hours to days before condensing into liquid form as precipitation.
When water vapor loses energy it "turns" into a liquid
when water vapour is cooled it condenses and falls as rain
Water can't condense. Condensation is about something turning from a gas to a liquid. Once it has become a liquid it can't be come liquid-er.
When water vapor condenses, it changes from a gaseous state to a liquid state. This process releases energy in the form of heat. The water molecules come together and form liquid droplets, which can be seen as clouds in the atmosphere or as dew on surfaces.
saturation point
Water vapor typically remains in the air for a few days before it condenses and forms clouds or precipitation.
When water vapor loses energy it "turns" into a liquid
Yes. There is latent heat release when vapor condenses.
When the temperature of water vapor condenses into a liquid, it is called condensation. This process involves the conversion of water vapor back into liquid water due to a decrease in temperature.
It condenses into liquid.
water vapor condenses to a liquid
When water vapor changes to liquid water, it condenses. This process releases latent heat energy into the surroundings.
Water evaporates into water vapour, and water vapour condenses into water.
Water vapor condenses into liquid water at its dew point temperature.
When water vapor condenses into liquid water, it changes from a gas to a liquid state. This process releases heat energy as the water molecules slow down and come closer together, forming liquid droplets.
When water vapor condenses into liquid water, it changes from a gas to a liquid state due to a decrease in temperature. This process releases energy in the form of heat, known as the latent heat of condensation. Condensation is responsible for the formation of clouds and precipitation in the atmosphere.
Condensation