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Fog and Clouds
Pictures: Fog moves through a gorge in Norway.
The Water CycleDuring its circulation, water changes its state regularly. It evaporates, because the sun heats it up, and so the liquid water becomes water vapour. This water vapour is absorbed by the air. Hot air can absorb more water vapour than cold air. So if a warm air current cools down, its ability to retain moisture, that is water vapour, declines and the water vapour has to escape in some way. This is brought about by condensation. The water vapour condenses on small dust or soot particles, which are called condensation nuclei in this connection, and forms small water droplets. This is nothing new to people wearing glasses. Surely they know the phenomenon where their glasses fog up as soon as they enter a warm room in winter. Here, exactly the same thing happens as described before. The warm, moist air comes in contact with the cold glasses, cools down and the water vapour has to escape. It condenses visibly on the glasses. Fog and Clouds - Same Material, Another Mode of FormationThe difference between fog and clouds is easy to explain. Clouds are formed when warm, moist air rises and afterwards cools down at high heights. The water vapour that was carried along condenses and clouds form. Depending on temperature and height, several types of clouds can form.
Fog: A 'low-lying' cloud!In contrast, fog forms when a warm and a cold air current, which are close to the ground, bump into each other causing the water vapour to condense. In other words, fog is nothing but a 'low-lying' cloud. Experiment: Formation of Clouds Material: a clear, transparent glass bottle with the cap, hot water, a metal lid, an old saucer, ice cubes, matches, paper.
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Last Update: 2004-Feb-29 |