Warm air rises at the equator and moves toward the poles while cold air sinks at the poles flowing back toward the equator. This creates Group of answer choices tornadoes. hurricanes. convection currents. the Coriolis effect.

Warm air rises at the equator and moves toward the poles while cold ai

1.	Warm air rises at the equator and moves toward the poles while cold air sinks at the poles flowing back toward the equator. This creates Group of answer choices tornadoes. hurricanes. convection currents. the Coriolis effect.
Answer» The development of weather patterns, such as CYCLONES and trade winds, are examples of the impact of the CORIOLIS EFFECT. ... As warm air rises near the Equator, for instance, it flows TOWARD the poles. In the NORTHERN Hemisphere, these warm air currents are deflected to the right (east) as they move northward.

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Warm air rises at the equator and moves toward the poles while cold air sinks at the poles flowing back toward the equator. This creates Group of answer choices tornadoes. hurricanes. convection currents. the Coriolis effect.

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