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19.2 Factors Affecting Winds
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The Coriolis Effect The tendency of an object moving freely over Earth’s surface to curve away from its path of travel
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Coriolis Effect
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Greatest near the poles; least near the equator
More Coriolis Effect To the right in the Northern Hemisphere; to the left in the Southern Hemisphere Greatest near the poles; least near the equator noaa.gov
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The faster the object, the greater the deflection
More Coriolis Effect The faster the object, the greater the deflection Not dependent on object’s movement direction
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More Coriolis Effect The effect is only noticeable for objects traveling over great distances, like an airplane or wind
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Coriolis Effect on Highs/Lows
Wind spirals clockwise out of high pressure; spirals counterclockwise into low pressure in our Hemisphere
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Slows down the air near Earth’s surface
Friction Slows down the air near Earth’s surface Force decreases with height, so winds increase with height
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The Polar-Front Jet Stream
Bands of swiftly moving winds near the top of the troposphere Divides cold air to the north, warm air to the south
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The Polar-Front Jet Stream
Supplies energy to storms and guides their paths Shifts south in winter, north in summer
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The Polar-Front Jet Stream
Discovered around WWII (1939) Allied bombers arrived early to their targets (tailwind); ground speed was very slow on return trip (headwind)—ran out of fuel
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Review Questions List 3 factors that affect wind direction.
Describe the path of air as it travels into a low-pressure area in the Northern Hemisphere. What effect could the polar-front jet stream have on the speed of an airplane flying eastward? An airplane flying westward?
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