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Just how does it work? Atmospheric pressure= 14.7 psi
Air Pressure Just how does it work? Atmospheric pressure= 14.7 psi
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Units of measure for Pressure
2 units for measuring pressure are, millibars, and inches of Mercury 29.73 997 30.18 994
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Which pressure gradient would result in greater wind velocity?
Isobars- iso is Greek meaning equal, bar is a unit of measuring pressure, so Isobars are lines of equal pressures
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Things that effect Air Pressure
Altitude (Elevation) Temperature Humidity (moisture in the air)
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Altitude The higher the altitude, the lower the air pressure. (less dense) The lower the altitude, the higher the air pressure. (more dense)
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Draw the relationship between air pressure and air density.
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Temperature As the temperature goes up, the air pressure goes down. (hot molecules are further apart- less dense, less pressure). As the temperature goes down, the air pressure goes up. ( cold air is more dense than warm air).
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Humidity Humidity is the amount of moisture in the air.
Water vapor weighs less than air molecules. As the air becomes more humid, the air pressure goes down (moist air weighs less than dry air). Drier air has higher pressure because dry air weighs more than moist air, therefore it has greater pressure.
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Winds Cause of wind
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Wind blows from areas of
to areas of high pressure low pressure
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How are winds named? The direction from which they come
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What instrument is used to measure:
wind speed air pressure anemometer barometer [ORIGIN from Greek anemos ‘wind’] [ORIGIN from Greek baros ‘weight’]
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How wind develops Caused by differences in air pressure, due to unequal heating of the atmosphere
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This is because the air is Therefore, clouds CANNOT form.
In a high pressure area, air will (rise, sink) because the air is (less, more) dense. This is because the air is (cold, warm) and (rises, sinks). Therefore, clouds CANNOT form.
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This is because the air is
In a low pressure area, air will (rise, sink) because the air is (less, more) dense. This is because the air is (cold, warm) and (rises, sinks). Therefore, clouds are LIKELY to form.
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Winds are created by… Heating the air, decreases pressure (warm air rises creating a low pressure) Cool air rushes in to replace the warm air (cooler dense air, produces high pressure) Winds form, as air goes from areas of high pressure to areas of low pressure
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Coriolis Effect Coriolis Effect Directions
Rotation of the Earth causes moving air and water to change direction Northern Hemisphere- winds curve to the right Southern Hemisphere- winds curve to the left
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Correctly draw the direction of wind flow
around both a high and a low pressure area in the NORTHERN HEMISPHERE. Counter- clockwise Clockwise
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counterclockwise wind direction
low pressure high pressure warm or cold air air rising or sinking clouds or no clouds clockwise or counterclockwise wind direction winds toward or away from the center warm cold rising sinking clouds no clouds counter clockwise clockwise toward away
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2 Types of Wind 1. Global 2. Local
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Global Winds Doldrums Trade Winds Prevailing Winds Polar Easterlies
Winds that blow over large distances. Do not travel North and South due to the Coriolis Effect 4 Types of Global Winds Doldrums Trade Winds Prevailing Winds Polar Easterlies
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Trade Winds Trade Winds
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Doldrums At the Equator, surface winds are calm and weak
Now known as, Intertropical Convergence Zone (ITCZ) At the Equator, surface winds are calm and weak Why would these winds be calm and weak? When would this cause a problem? ITCZ
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Trade Winds 30 degrees North and South of the Equator
Calm Winds, few clouds, little rain fall Warm air rising from the equator cools and sinks Also known as the Horse Latitudes
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Prevailing Westerlies
Strong Winds Located in the belt degrees latitude in both Hemispheres Has an impact on the US weather Is the prevailing wind in the United States
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Polar Easterlies Cold, but weak winds Near the North and South Poles
US weather is influenced by these Cooling takes place between the degree latitude as it approaches the poles
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Jet Stream Discovered in the 1940’s
Can be found in the upper Troposphere Strong, high speed and high pressure Moves West to East across the US, moving storms
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Local Winds Cover short distances and blow from any direction
2 Types of Local Winds Sea Breezes- from sea to land Land Breezes- from land to sea
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Sea Breeze
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Land Breeze
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