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The Coriolis effect
Global winds
Wind
Equator and 30 degrees
Jet Stream
The effect of Earth's rotation on the direction of winds and currents.
False
Convection
Westerlies
The transfer of thermal energy by the circulation or movement of a liquid or gas
Global winds
Wind
Equator and 30 degrees
Jet Stream
The effect of Earth's rotation on the direction of winds and currents.
False
Convection
Westerlies
a high-speed high-altitude airstream blowing from west to east near the top of the troposphere
Global winds
Wind
Equator and 30 degrees
Jet Stream
The effect of Earth's rotation on the direction of winds and currents.
False
Convection
Westerlies
Wind is caused by the rotation of the earth.
Global winds
Wind
Equator and 30 degrees
Jet Stream
The effect of Earth's rotation on the direction of winds and currents.
False
Convection
Westerlies
Trade Winds are found between these latitudes
Global winds
Wind
Equator and 30 degrees
Jet Stream
The effect of Earth's rotation on the direction of winds and currents.
False
Convection
Westerlies
The uneven heating of planet earth by the sun causes
Global winds
Wind
Equator and 30 degrees
Jet Stream
The effect of Earth's rotation on the direction of winds and currents.
False
Convection
Westerlies
prevailing winds that blow from west to east between 30 degrees and 60 degrees latitude in both hemispheres
Global winds
Wind
Equator and 30 degrees
Jet Stream
The effect of Earth's rotation on the direction of winds and currents.
False
Convection
Westerlies
Winds that blow steadily from specific directions over long distances
Global winds
Wind
Equator and 30 degrees
Jet Stream
The effect of Earth's rotation on the direction of winds and currents.
False
Convection
Westerlies
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