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15.3 Global Winds & Local Winds

AB
windthe movement of air caused by differences in air pressure
coriolis effectthe apparent curving of the path of a moving object from an otherwise straight path due to the earth's rotation
polar easterliesprevailing winds that blow from east to west between 60 degrees and 90 degrees latitude in both hemispheres
westerliesprevailing winds that blow from east to west between 30 degrees and 60 degrees latitude in both hemispheres
trade windsprevailing winds that blow from northeast from 30 degrees north latitude to the equator and that blow southeast from 30 degrees south latitude to the equator
jet streama narrow belt of strong winds that blow in the upper troposphere
convection cellsair that travels in large, circular patterns
pressure beltsbands of high pressure and low pressure found about every 30 degrees of latitude



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