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Wind
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Wind Formation Differences in temperature causing differences in pressure high to low Winds are named for where they come from
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Instruments Wind vane Direction Anemometer Speed
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Types of Local Winds Sea breezes and land breezes Sea Breeze
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Land breeze
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Coriolis Effect Due to earth’s rotation
Fluids in the N.H. are deflected to the right Opposite in the S.H.
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No Rotation Rotation L L H H
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Hurricane in the Northern Hemisphere *
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Hurricane in the Southern Hemisphere
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Global Wind Patterns
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Global Wind Patterns
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Rising air = low pressure = clouds = wet climates
Sinking air = high pressure = no clouds = dry climates
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Jet Stream Strong winds in the upper troposphere “rivers of air”
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Jet Stream *
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