Water vapor condenses into liquid water at its dew point temperature.
Water vapor in air condenses into liquid water at the dew point temperature.
Water vapor needs to cool down in order to turn into droplets. This cooling process can happen by either coming into contact with a colder surface or by the surrounding air temperature dropping. Once the water vapor cools sufficiently, it will condense into droplets.
Water vapor in the air can condense on a cold window, forming droplets. This is because the cold temperature causes the water vapor to cool and change from a gas to a liquid state.
If the water vapour comes in contact with a surface and is allowed to cool and condense, it will turn back to liquid. For example, if you were to boil a pot of water with a lid on top, the water vapour would rise, touch the underside of the pot lid and condense to form droplets (liquid).
When you exhale warm, moist air onto a cold window, the air cools rapidly upon contact with the cold surface. This causes the water vapor in your breath to lose heat energy and condense into tiny water droplets on the window, creating fog or frost.
Water vapor in air condenses into liquid water at the dew point temperature.
Actually, the temperature at which water vapor begins to condense into liquid water is called the dew point. It is the temperature at which air becomes saturated with moisture.
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The temperature at which vapor starts to condense is called the dew point temperature. This is the temperature at which the air becomes saturated with water vapor and condensation begins to form.
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True. The dew point is the temperature at which air reaches saturation and water vapor in the air begins to condense into liquid water on surfaces.
Water vapor is already a gas since it is the gaseous form of water. If you are referring to how water vapor turns into liquid water, it does so through condensation when the temperature decreases enough for the vapor to condense back into liquid form.
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Water vapor condenses into liquid water when it reaches the dew point temperature, which is the point at which the air becomes saturated with moisture and cannot hold any more water vapor. This temperature can vary depending on factors such as air pressure and humidity levels.
Water vapor in air condenses when the air temperature drops below the dew point temperature, causing the water vapor to change from a gaseous state to a liquid state. This typically happens in the atmosphere when air is cooled, such as during the night or when warm air rises and cools at higher altitudes.
When water temperature reaches the dew point, water vapor in the air starts to condense into liquid water droplets. This process forms dew on surfaces like grass or windows.
0 degree centigrade after giving the latent heat.