You are here

Cloud formation draft

Submitted by zalam on Mon, 11/04/2019 - 10:34

When the sun heats up several water bodies, water vapor starts rising up due to its low density. As it reaches a higher altitude, the temperature starts to cool down. This drop results in the vapor to condense and form clouds above. A more simplified version can be shown using a cloud in a bottle. Adding a small amount of water (or to make the process much faster - ethanol) in a 1 litre plastic bottle would represent the process in a closed system. Using a rubber cork, the nozzle of an air pump can be secured in place. Once everything is set, air is pumped into the bottle with water/ethanol. As more air is pumped into the bottle, the pressure inside starts increasing. Since PV=nRT, the temperature also starts to rise inside. This equates to the water rising once the sun heats up the seas, lakes, rivers etc. As soon as the cork is removed, there is a pop sound following by a sudden appearance of fog, which represents the cloud. When the cork is removed, there is a sudden drop in pressure, followd by the drastic drop in temperature that rapidly cools down the heated air inside, thereby causing condensation.  

Post: