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Atmospheric Pressure and Winds Chapter 19
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Air Pressure The weight of the atmosphere per unit area. –1kg per cm² at sea level –14.7 lbs/in² at sea level Directed equally in all directions Barometer – 76cm / 30in at sea level – given in metric unit of millibars (mb)
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Barometer Instrument that measures air pressure Mercury Barometer –Requires a tall column of mercury Aneroid Barometer –Uses no liquid
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Mercury Barometer
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Air Pressure Records
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Why Air Pressure Changes Temperature Changes – warm air is lighter than cold air Changing Humidity – the more water vapor, the lighter the air – water vapor pushes out heavier O 2 and N 2 of the dry air
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What Makes Wind Blow Pressure Gradient Force – the difference in air pressures that cause winds Local Winds – Sea Breeze: daytime wind from sea, land heats faster than water and causes air to rise – Land Breeze: nighttime wind from land to sea, water is warmer than land
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Local Winds: Sea Breeze
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Local Winds: Land Breeze
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Earth’s Rotation and Weather Systems Coriolis Effect –Turns wind to the right Clockwise –Out of HIGH pressure Counterclockwise –Into LOW pressure
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High Pressure Center
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Low Pressure Center
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Global Air Currents
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Air Masses and Fronts Chapter 20
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Air Masses Huge section of air that has the same weather throughout Take on the characteristics of the area they originated over maritime tropical – mT continental tropical – cT maritime polar – mP continental polar - cP
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Air Mass Source Regions
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Fronts Boundary between 2 air masses Causes warm air to rise –Where temperatures and humidity change
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Warm Front: Map View Slow moving Long lasting rain Cirrus to stratus clouds, then nimbostratus
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Warm Front: Side View
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Cold Front: Map View Fast moving Unstable air Cumulus – cumulonimbus clouds Thunderstorms Clears quickly and leaves clear skies
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Cold Front
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Occluded Front: Map View When a cold front overtakes a warm front Form low pressure systems
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Occluded Front: Side View Warm Air Cold Air
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