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Published byArthur Griffin Modified over 8 years ago
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Air Pressure & Wind Patterns
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What is air pressure? Air pressure is the force of molecules pushing on an area. Air pressure pushes in all direction Why don’t you feel air pressure since its so heavy? Air pressure pushes in ALL directions, so the force up is also equal to the force pushing down.
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Air Pressure and altitude Air pressure decreases as you move higher in the atmosphere, due to less air above you Density also decreases air pressure. Air at sea level is more dense than at high altitudes
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Air Pressure As altitude increases, air pressure decreases. Air pressure also decreases as the amount of water vapor in the air goes up. Warm air is less dense than cool air, so when temperatures are higher, the air pressure is usually lower.
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Uneven heating causes air to move Weather is the Earth’s atmosphere at a particular time. Wind is air that moves horizontally or parallel to the ground. Uneven heating of the surface causes PRESSURE DIFFERENCES, which create wind. Wind always moves HIGH TO LOW PRESSURE!!!!!
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What factor determines wind strength? The difference in air pressure between two areas determines the strength of the wind.
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Global winds Can travel thousands of kilometers in steady patterns. Caused by uneven heating of equator and north and south pole Influence of Earth’s rotation of the wind is called the Coriolis effect.
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Bands of calm air separate global wind belts
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Calm Regions Doldrums low pressure zone near the equator Horse latitudes are high pressure zones 30 degrees north and south of the equator
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Wind Belts Trade winds blow from the EAST, moving from horse latitude to equator. Westerlies blow from the WEST, moving from horse latitudes to the poles Easterlies blow from the EAST moving from polar regions toward mid-latitudes. Storms form when cold easterlies meet warm westerlies
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Jet streams Jet Streams flow in the upper troposphere from WEST to EAST. Moves as fast as 124 miles/hour. Jet streams are used to make weather predictions.
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Local Winds Warm air rises over land during the day Warm air rises over the ocean at night.
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Monsoons Monsoons are winds that change direction with the seasons. Caused by the different heating and cooling rates of land and sea.
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Temperature affects water in the air. EVAPORATION is the process which a liquid can change into a gas, this requires extra energy Condensation is the process by which a gas changes into a liquid, occurs when moist air cools.
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WATER CYCLE…. When air rises in the atmosphere it cools, condensing into ice crystals or water droplets. When the droplets or ice crystals get heavy enough, they fall to the ground as precipitation.
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Humidity & Relative Humidity Humidity is the amount of water vapor in the air, caused by the lack of evaporation. Saturation is a condition in which the rates of evaporation and condensation are equal. Relative humidity compares the amount of water vapor in air with maximum amount of water vapor that can be present at that temperature. Dew point is the temperature at which air with a given amount of water vapor will reach saturation. Higher the DP of air, the more water vapor.
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Clouds are made of CONDENSED water vapor
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rm is approaching.
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Cumulus Clouds Cumulus Clouds Puffy white clouds with dark bases. Appear in fair weather. If they grow tall, they produce storms.
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Stratus Clouds. Stratus Clouds Smooth clouds, form with no air movement. Can produce steady, light precipitation.
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Fog FOG clouds that rest on the ground or a body of water. Forms when surface is colder than the air above it.
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TYPES OF PRECIPITATION Rain and Drizzle- Most common. Water droplets or ice crystals melting as they fall, usually in stratus clouds. Freezing Rain - Rain that freezes when it hits the ground. Sleet - Rain the freezes into ice pellets while falling in cold air. Snow - Forms from ice crystals that merge in clouds Hail - Forms when ice pellets move up and down in clouds, growing larger as they gain layers of ice.
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