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Weather Concepts Air Masses Air masses are large bodies of air that have the same temperature and humidity throughout They can form over land or water They can range from 100 km to 1000 km in size Air Masses A warm air mass consists of warm air and it can be dry or humid If the air mass forms over warmer oceans then the air mass will be humid (maritime tropic) If the air mass forms over land then the air mass will be dry (continental tropic) Air Masses A cold air mass consists of cold air and it can be dry or humid If the cold air mass forms over cold ocean water then it will be humid (maritime polar) If the cold air mass forms over cold land then it will be dry (continental polar) Any air mass that forms over the Arctic is very cold and very dry Fronts Cold air masses from the north and warm air masses from the equator move towards each other When these mass collide they create fronts The difference in temperatures found between the air masses creates a boundary Fronts Warm front occurs when a warm air mass comes into an area and pushes the colder air up and out. This front brings periods of light rain. Cold front occurs when a cold air mass comes into an area and pushes a warm air mass up quickly. This front usually brings thunderstorms or very heavy rain. Fronts Occluded front occurs when a fast moving cold air mass collides with a warm front and forces it upwards. As a result the cold air mass catches up to the other cold air mass on the other side of the front. This type of front can sometimes bring thunderstorms but usually results in drying of the air mass Fronts Stationary front occurs when a a cold air mass meets a warm air mass but does not move. This type of front brings cloudy skies and precipitation (usually lighter rain) for longer periods of time Types of Fronts http://www.phschool.com/atschool/phsciex p/active_art/weather_fronts/ Pressure Systems A low pressure system forms as a warm air mass travels over warm land or oceans The air flows up and away from earth’s surface which lowers the pressure on the earths surface Water vapor condenses and precipitation can be expected Pressure Systems A high pressure system forms over a cool ocean or land and can be very large The dense air falls towards the earth’s surface causing the air pressure to increase As the high pressure air falls to earth it becomes warmer and drier It normally brings sunny and clear skies