Air Pressure and Wind

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jh4hatchett1  on May 1, 2012

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Air Pressure and Wind

Pressure Gradient Force
amount of pressure change over a givn distance
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Pressure Gradient Force amount of pressure change over a givn distance
isobar line connecting points of equal pressure
altitude as this increases air pressure decreases
divergence must occur alof for a low pressure system to exist
cyclone low pressure center
monsoon seasonal change in wind related to heating and cooling of a landmass
wind horizontal movementof air from areas of low pressure
subtropical high located around 30 degrees latitude
sea breeze occurs durring the day and blows onshore
equator where there is no coriolis effect
troposphere atmospheric layer where the jet streams are found
equatorial low pressure zone characterized by rising air and abunndant precipitation
aneroid small portable barometer
cupanerometer measures wind velocity
torricelli devised first mercury barometer
high pressure expect fair weather when this approaches
polar high gives rise to polar easterlies
air pressure force exerted by the force of air above
wind speed what the coriolis effect is proportional to
wind vain measures wind direstion
geostrophic winds that are unaffected by friction from the earths surface
jet stream fast moving river of air that moves weather
anticyclone high pressure center
westerlies prevailing winds that affect most of the US
coriolis apparent deflective force of earth's rotaion
counter-clockwise dirction that an anticyclone rotates in the southern hemisphere

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jh4hatchett1