Ch6 meteorology Air pressure and winds

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Last updated 6:45 PM on 4/3/26
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16 Terms

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how does atmospheric pressure affect wind?

Wind is the result of horizontal differences in atmospheric pressure

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atmospheric pressure

the force exerted against a surface by continuous collision of gas molecules

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Measuring Air Pressure

Air pressure is measured in millibars (mb), where 1 millibar is equal to 100 newtons/m^2

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Mercury Barometer

An instrument that measures changes in air pressure, consisting of a glass tube partially filled with mercury.

- Air pressure pushes on a pool of mercury, which forces the mercury up a tube

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Pressure Changes with Altitude

Air pressure is defined as the force exerted against a surface by continuous collision of gas molecules

Air pressure decreases with altitude

Air pressure increases with depth

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Why does air pressure vary?

Altitude, Temperature, Humidity, Movement of air masses

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how does moisture affect air pressure?

- the amount of water vapor reduces the density of air

- cold hair has higher pressure

- warm, dry air has higher pressure compared to moist air

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Convergence/Divergence and Air Pressure

-Convergence occurs when a net airflow causes pressure to rise

- Divergence results when there is a net outflow of air from a region and surface pressure drops

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Factors affecting wind

1. pressure gradient force

2. coriolis effect

3. friction

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Pressure Gradient Force

Drives air from areas of higher barometric pressure to areas of lower barometric pressure, causing winds.

<p>Drives air from areas of higher barometric pressure to areas of lower barometric pressure, causing winds.</p>
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Coriolis Effect and how it effects wind

-Doesn't generate wind, only modify airflow

- In northern hemisphere, deviates to the right

- in southern hemisphere, deviates to the left

<p>-Doesn't generate wind, only modify airflow</p><p>- In northern hemisphere, deviates to the right</p><p>- in southern hemisphere, deviates to the left</p>
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Friction in Wind

- Friction significantly influences airflow near Earth's surface, but its effect is negligible at higher altitudes.

- Slows down the air speed causing a reduction in the Coriolis effect, allowing the wind to cross the isobars at an angle-

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Geostrophic Flow

occurs when the pressure gradient force and the Coriolis force are balanced.

<p>occurs when the pressure gradient force and the Coriolis force are balanced.</p>
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curved airflow

winds around cells of high pressure or low pressure follow curved paths

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cyclone/anticyclone

Cyclone: A low pressure region with an accompanying surface wind Anticyclone: a high pressure system with accompanying winds

<p>Cyclone: A low pressure region with an accompanying surface wind Anticyclone: a high pressure system with accompanying winds</p>
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cyclone and anticyclone at north and south hemispheres

Northern hemisphere: Counterclockwise

Southern hemisphere: Clockwise

<p>Northern hemisphere: Counterclockwise</p><p>Southern hemisphere: Clockwise</p>

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