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As the sun heats the water, more rapid motion of the water molecules begins. Several these rapidly moving molecules succeed in removing themselves of the water belo...

Through our atmosphere water vapor is being an invisible gas present. Through evaporation from the seas about ninety days of the water vapor joins the earth's atmosphere. As the ocean waters get heat from the sun, a part of the water turns from a fluid to a and in the hot water that gas increases.

More rapid motion of the water molecules starts, while the sun heats the water. Numerous these rapidly moving molecules succeed in removing themselves of the water below and as water vapor they run away.

However the capacity of air to keep water vapor is not unlimited. On the air temperature depend just how much it could carry. For warmer air the capacity to carry water vapor is more. As the limit it reaches no further water vapor it can hold, that's, it's saturated, or the saturation point it has achieved. Beyond this stage, the water vapor will start returning to liquid form through condensation.

Once the water vapor starts condensing that very temperature level is known as the dewpoint here. For the condensation process dirty air development above walk out is the need really. Particles like dirt, salt, and suspended pollutants fill out the atmosphere we reside in. As these products perform since for the water vapor molecules to clump around they locate a part condensation nuclei.

Condensation just above the bottom is behind haze formation. Clouds are produced by condensation at higher levels. It is quite reasonable to feel that fog is just a cloud on the floor level, because the process for each is completely identical with the other.

Formation of cloud

Are formed when condensation happens above walk out clouds. Water vapor condenses into water droplets when the surrounding air temperature is above freezing point. Nevertheless when air temperature below freezing point dominates water might sublimate or change into ice crystals. Sometimes in a state below freezing the water vapor may stay.

Since broadly speaking with elevation temperature decreases, large level clouds have tendency to make into ice crystal clouds while low level clouds could become water droplet clouds, often a combination comes of middle level clouds. Hundreds of millions of droplets and/or ice deposits join to make clouds. On numerous factors depends the cloud type.

For the rise of the air masses three processes work. Of those convection may be the first. Whilst the sun heats the surfaces the air above the surfaces begins increasing since that air also gets heated. Soil, mud and pavement are some of the surfaces that heat up faster for their efficiency in the problem. Every where these warm bodies of air start to rise, they ultimately achieve the dewpoint and cloud formation may be the result.

When crash of fronts occur the rise of air is also possible. Cloud development takes place if in the hot air enough moisture occurs.

Raising of air can be possible when it looks mountain ranges and other geographical features. More, clouds will form if enough water is present in the raised air. Unusual cloud forms are often resulted from orographic lifting.

The rise of an air mass remains as long as according of the surrounding air it is hotter. Stability was not got by the conditions still the rise continues. Nevertheless, with balance steady conditions are quickly reached. Generally, the conditions are unstable if over hot air exists cool air in the upper atmosphere. When warm air has ended cold air, steady circumstances result broadly speaking. e smoke info