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Since the wind belts rely on the earth's rotation, certain areas on earth would be really hot and other areas would be frigid. Also the extreme areas on earth would become more extreme and some areas would have lots of disasters such as flooding and hurricanes.

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The westerlies cover the area in which the Lisle community is located.

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Since Chicago-land is near the Jet Stream, the jet stream influences the weather in the area. In the summer the jet stream is north of Chicago so the temperature is warmer since the jet stream circulates warm air whereas in the winter since the jet stream is south of Chicago, the weather is much colder since the jet stream circulates the cold air in the winter.

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Jet Streams flow from West to East- the same direction the Earth Rotates. The jet stream speed is average 300km/h and can reach 500km/h. The surface wind average is between 20 and 30km /h

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Jet streams form where global wind belts meet and bring warm and cold air together.

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Between 30' & 60' N&S
Winds blow east ward from the horse latitudes. These winds can also heat and when they reach about 60' N&S the winds head towards the equator.

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60'N &S
warm air moving from the lower latitudes rises and forces the cool air to rise

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- 30' N and 30' S
- Air is cooled, increases in density, stops moving towards the poles & sinks.
- High pressure & calm air
- Little Rain
Between Equator and 30'N & S
Blow westward & toward the equator
Steady

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1. Intertropical Convergence Zone - aka doldrums

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1. Intertropical Convergence Zone - aka doldrums

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Equator, Low-pressure zone. The winds from the northern and southern hemisphere converge here.

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Winds are caused by differences in air pressure from one area to another.

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Due to there being less solar radiation at the poles, the air is colder and heavier. This air sinks and creates regions of high pressure.

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Due to the solar radiation from the sun, the air at the equator is heated and rises consistently so there is an area of low air pressure at the equator.

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The circulation of heat in an area.

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The direct transfer of heat from one substance to another substance through contact.

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The movement of air from an area of high pressure to an area of lower pressure.