This is some info on condensation
Condensation is the change of water from its water vapour into liquid form. Condensation generally occurs in the atmosphere when the warm air rises but later cools which loses the capacity to hold the water vapour. Which then turns into cloud droplets (clouds).
You don't have to look at something as far away as a cloud to notice condensation, though. Condensation is responsible for ground-level fog, for your glasses fogging up when you go from a cold room to the outdoors on a hot and humid day. It is also responsible for the water that drips off the outside of your glass of iced tea, and for the water on the inside of the windows in your home on a cold day. Condensation is the opposite of Evaporation.
As condensation occurs water forms from the vapour, the water molecules become organized in a less random structure, which is less random than in vapour, and heat is released into the atmosphere as a result.
Condensation also occurs at ground level, the difference between fog and clouds which form above the Earth's surface is that rising air is not required to form fog.
Another way in which condensation occurs is on hard surfaces, such as during the formation of dew. Water condensing on a glass of ice water, or on the inside of windows during winter
Condensation is the change of water from its water vapour into liquid form. Condensation generally occurs in the atmosphere when the warm air rises but later cools which loses the capacity to hold the water vapour. Which then turns into cloud droplets (clouds).
Have you ever noticed the droplets of water that form on the outside of a canned drink when you take it out of the fridge? This is condensation and the reason why it happens is all to do with temperature, air and water vapour.
The temperature on the surface of the can is reduced as air passes over it. As the air gets cooler its relative humidity rises and the water vapour turns into moisture. The air passing over the can is unable to hold onto the moisture which ends up as droplets running down the side of the can’s cold surface.
Condensation is the change of water from its water vapour into liquid form. Condensation generally occurs in the atmosphere when the warm air rises but later cools which loses the capacity to hold the water vapour. Which then turns into cloud droplets (clouds).
You don't have to look at something as far away as a cloud to notice condensation, though. Condensation is responsible for ground-level fog, for your glasses fogging up when you go from a cold room to the outdoors on a hot and humid day. It is also responsible for the water that drips off the outside of your glass of iced tea, and for the water on the inside of the windows in your home on a cold day. Condensation is the opposite of Evaporation.
As condensation occurs water forms from the vapour, the water molecules become organized in a less random structure, which is less random than in vapour, and heat is released into the atmosphere as a result.
Condensation also occurs at ground level, the difference between fog and clouds which form above the Earth's surface is that rising air is not required to form fog.
Another way in which condensation occurs is on hard surfaces, such as during the formation of dew. Water condensing on a glass of ice water, or on the inside of windows during winter
Condensation is the change of water from its water vapour into liquid form. Condensation generally occurs in the atmosphere when the warm air rises but later cools which loses the capacity to hold the water vapour. Which then turns into cloud droplets (clouds).
Have you ever noticed the droplets of water that form on the outside of a canned drink when you take it out of the fridge? This is condensation and the reason why it happens is all to do with temperature, air and water vapour.
The temperature on the surface of the can is reduced as air passes over it. As the air gets cooler its relative humidity rises and the water vapour turns into moisture. The air passing over the can is unable to hold onto the moisture which ends up as droplets running down the side of the can’s cold surface.