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Air Masses and Fronts Page 128 •Climate is what we expect, weather is what we get • Mark Twain Air Mass page 129 • A large body of air throughout which temperature and moisture content are similar • The amount of solar energy received and location of formation determines the temperature and moisture content in the air mass. Types of Air Masses-Moisture 1. Continental Air Masses – form over land masses. Dry (not a lot of water). 2. Maritime Air Masses – form over oceans or other large bodies of water. Wet (moisture amount depends on solar energy). Types of Air Masses-Temperature 3. Tropical Air Masses – form in warm regions, contain hot or warm air (lots of solar energy) 4. Polar Air Masses – form in cold regions, contain cold or cooler air. (less solar energy) Always has a moisture and temperature indicator! Air masses Source Region Type of air Symbol Continental Dry c Maritime Moist m Tropical Warm T Polar Cold P Front page 130 • A boundary between air masses, where the air does not usually mix • The differences in temperature and pressure cause clouds and precipitation to form at fronts • We map these boundaries to find out what the weather will be like in different areas of the world Cold Front • The front edge of a moving mass of cold air that pushes beneath a warmer air mass like a wedge. • Heavy precipitation or thunderstorms form at this boundary and it brings colder weather Warm Front • The front edge of an advancing warm air mass that replaces colder air with warmer air • Produces precipitation over a large area, followed by clear skies Stationary Front • The front edge of two air masses that meet and move either very slowly or not at all • Varied weather, but usually clouds and precipitation Occluded Front • Cold air mass that overtakes a warm air mass and lifts the warm air mass off the ground and over another cold air mass • Weather is variable with some areas stormy and others not