Bentzen Chapman

As the sun heats the water, more rapid movement of the water molecules starts. Lots of these rapidly moving molecules flourish in removing themselves of-the water belo...

Through our atmosphere water vapor exists as an invisible gas. Through evaporation from the oceans about 3 months of the water vapor joins the earth's atmosphere. As the sea waters get heat from the sun, an integral part of the water transforms from a fluid to a gas and in the hot water that gas increases.

While the sun heats the water, faster motion of the water molecules begins. Several of the rapidly moving molecules succeed in removing themselves of the water below and as water vapor they try to escape.

However the capacity of air to carry water vapor is not unlimited. About the air temperature count simply how much it can carry. For warmer air the capability to carry water vapor is more. As it reaches forget about water vapor it can take, that's, it's unhealthy the limit, or the saturation point it has reached. Beyond this point, the water vapor will start coming back to liquid form through condensation.

When the water vapor begins condensing that very temperature level is recognized as the dewpoint here. For the condensation process dirty air development above ground level may be the need really. Particles like salt, dust, and suspended pollutants fill out the atmosphere we live in. As these products work since for your water vapor molecules to clump around they locate a role condensation nuclei.

Condensation just above the ground is behind fog formation. Clouds are created by condensation at higher levels. Because the process for every single is absolutely identical with the other, it is very logical to believe that fog is just a cloud on the floor level.

Formation of cloud

When condensation takes place above ground level clouds are formed. When the surrounding air temperature is above freezing point water vapor condenses in to water drops. However when air temperature below freezing point prevails water may possibly sublimate or change directly into ice crystals. Sometimes in a state below freezing the water vapor can remain.

Since usually with elevation temperature decreases, high level clouds have tendency to create into ice crystal clouds while low level clouds can become water droplet clouds, usually a combination comes of middle level clouds. Hundreds of millions of droplets and/or ice crystals