In a midlatitude cyclone, air is drawn toward the center of low pressure from both the warm and the cold sides of the polar front.

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Quizplus · Accepted Answer

In a midlatitude cyclone, air is indeed drawn toward the center of low pressure from both the warm and the cold sides of the polar front. This is because the polar front is the boundary between colder polar air and warmer subtropical air, and the cyclone forms due to the interaction between these two air masses. As the low pressure system develops, air is pulled in from all sides, creating the swirling pattern characteristic of a cyclone.

In a Midlatitude Cyclone, Air Is Drawn Toward the Center