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TOC: Winds 2-8-13 I STARTER: Think back to the demos, does air move from low pressure to high pressure or the other way around?? Explain…..

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Presentation on theme: "TOC: Winds 2-8-13 I STARTER: Think back to the demos, does air move from low pressure to high pressure or the other way around?? Explain….."— Presentation transcript:

1 TOC: Winds 2-8-13 I STARTER: Think back to the demos, does air move from low pressure to high pressure or the other way around?? Explain…..

2  The movement of air in a horizontal direction II: Practice-Notes What is a wind??

3  The uneven heating of the Earth causes differences in air pressure. What causes wind?

4  The Sun’s energy is more concentrated at the Equator and spread out more over the poles.  Air over the equator is warm and less dense and has lower pressure.  Air over the poles is cold and denser and has higher pressure. Why does this happen?

5  As warm air at the equator rises, cooler air from the poles will move in and replace it.  Air pressure moves in a pattern from high to low. Why does this happen?

6  As warm air at the equator rises, cooler air from the poles will move in and replace it. Convection

7  The density changes caused by temperature changes create convection cells.  These cause circular patterns of air that circulate over the whole planet. Global Convection Currents

8  Where the convections cells meet, prevailing winds and jet streams form.  They blow from one direction over a certain area of the Earth’s surface. Global Wind Belts

9 Jet Stream

10  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.

11 Jet Stream Animation http://www.pbs.org/wgbh/nova/vanished/jetstr_five.html

12  Named for the direction from which they blow:  Polar Easterlies  Polar Easterlies – High latitudes blow east to west toward the equator  Westerlies  Westerlies – Mid latitudes blow west to east toward the poles  Easterlies (Trade Winds)  Easterlies (Trade Winds) – Low latitudes blow east to west toward the Equator Prevailing Winds

13

14 0 o Equator 30 o S 60 o S 90 o S 30 o N 60 o N90 o N More Direct Sun Hot

15  The winds from the poles blow toward the equator.  The winds from the equator blow toward the poles. Global Wind Belts

16  As the Earth rotates counterclockwise, the winds bend and curve around the Earth.  Coriolis, an engineer and mathematician, described this effect as an inertial force in 1835. The Coriolis Effect

17  In the Northern Hemisphere, winds bend to the right of their direction of travel.  In the Southern Hemisphere, winds bend to the left of their direction of travel. The Coriolis Effect

18  Weather patterns and systems move in a circular motion due to the bending of the winds caused by the Earth’s rotation. The Coriolis Effect

19  Let’s try a little investigation to see how the Coriolis Effect works.  Follow the directions on your handout, except we will be using a paper plate instead of cutting out the circle…  Answer the questions here!!! III Application:

20 Describe how winds are produced and why they do not blow directly from the poles to the equator and back. Describe how winds are produced and why they do not blow directly from the poles to the equator and back. IV Connection/ V Exit:


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