Atmospheric movement ppt cscope

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Transcript of Atmospheric movement ppt cscope

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0 o Equator 30 o S 60 o S 90 o S 30 o N 60 o N 90 o N

MoreDirect Sun Hot

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*Forms high in the upper Troposphere between two air masses of different temperatures *Higher temperature difference = faster speed *Due to the Coriolis Effect, it flows around air masses. *Polar Jet: *It dips southward when frigid polar air masses move south. *It tends to stay north in the summer months

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http://www.pbs.org/wgbh/nova/vanished/jetstr_five.html

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Abnormally high surface ocean temperatures off the coast of South America

Causes unusual weather patterns

across the globe

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*A strong surface current *Begins at the tip of Florida *Flows up the eastern coastline of the U.S. *Crosses the Atlantic Ocean *Causes warmer climate in NW Europe

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*Why does the Earth have wind and ocean currents?

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*When convection and winds cause air masses to move, they bump into one another.

*The area where two air masses meet is called a front.

*Most severe weather occurs near frontal boundaries.

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*Warm and cool air masses that are not strong enough to move one another

*Sits still for a long period of time

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http://www.stevemcentee.com/animation3.html

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*Air pressure is measured with a barometer in millibars.

*Millibars are represented by connected lines of equal pressure. This is a lot like the topographic map lines.

*The closer together the lines are, the faster the wind speed.

*The farther apart the lines are, the slower the wind speed.

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*The Sun heats the water and land every day.

*Land heats up rapidly, but cools off rapidly.

*Desert

*Water heats up slowly, but cools off slowly.

*Swimming at night

*The heat retained by the oceans is what keeps our planet insulated.

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*The heating and cooling of water and land produces land breezes and sea breezes.

*High pressure moves toward low pressure, pushing the warm air upward.

*As warm air rises, cooler air moves in and replaces it.

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*How do global patterns of atmospheric movement affect local weather?