Atmospheric Circulation

Temperature differences between different regions of the Earth's surface create pressure differences, which in turn drive atmospheric circulation.

Jet streams are not a major type of global wind pattern, but rather a narrow band of strong winds in the upper atmosphere.

The Westerlies are a global wind pattern that flows from the northeast to the southwest in the Northern Hemisphere.

Wind patterns are a result of atmospheric circulation, not a factor that influences it.

The Trade winds are a global wind pattern that flows from the southeast to the northwest in the Southern Hemisphere.

Cyclone is a type of weather system, not a type of pressure system.

The Trade winds are a global wind pattern that flows from the east to the west in the tropics.

Heavy precipitation is a characteristic of a low-pressure system, not a high-pressure system.

The Westerlies are a global wind pattern that flows from the west to the east in the middle latitudes.

Clear skies are a characteristic of a high-pressure system, not a low-pressure system.

The Polar easterlies are a global wind pattern that flows from the north to the south in the polar regions.

Wind patterns are a result of atmospheric circulation, not a factor that influences its strength.

The Polar easterlies are a global wind pattern that flows from the south to the north in the polar regions.

Walker cell is a type of ocean circulation cell, not an atmospheric circulation cell.

The Trade winds are a global wind pattern that flows from the west to the east in the tropics.