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Guide to Weather
Weather Basics
Understanding Weather
Air Temperature
Air Pressure
Wind Speed & Direction
Precipitation
Humidity & Dew Point
Clouds & Visibility
Forecasting
Effects
Frequently Asked Questions
Glossary
 

 Understanding Clouds & Visibility

A cloud is simply a big group of water molecules or ice particles in the form of water vapor that stays clumped together and floats in the air above the earth. Clouds most often form as the result of air rising from the earth in one of these ways:
Convection: The heating of the ground creates bubbles of warm air that rise into the atmosphere.
 
Topographic Lifting: The lifting of air up the side of a mountain. The windward side of a mountain (the side that the wind is blowing against) tends to have more clouds than the leeward side (the side facing away from the wind).
 
Convergence: The meeting of air from several different directions at the earth's surface near low pressure systems. A hurricane (over water) is an example of a low pressure center that causes air to converge at the earth's surface, resulting in severe thunderstorms over land.
 
Frontal Lifting: The lifting of air along a frontal boundary (the front of a storm, for example). Cold fronts and warm fronts force air to rise. The most dramatic cloud formations result from a cold front, because the slope of the front is steeper than a warm front.
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