In the Northern Hemisphere, around a low-pressure center, wind generally flows how?

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Multiple Choice

In the Northern Hemisphere, around a low-pressure center, wind generally flows how?

Explanation:
In the Northern Hemisphere, a low-pressure center draws air inward and wind flows counterclockwise around it. This happens because air moves from higher to lower pressure (the pressure gradient force) toward the center, and as it does, the Coriolis effect bends the motion to the right. The result is a spiraling inward flow that is counterclockwise around the low. This inward, cyclonic circulation is the defining pattern around a low in the NH, whereas a high pressure center would produce a clockwise, outward flow.

In the Northern Hemisphere, a low-pressure center draws air inward and wind flows counterclockwise around it. This happens because air moves from higher to lower pressure (the pressure gradient force) toward the center, and as it does, the Coriolis effect bends the motion to the right. The result is a spiraling inward flow that is counterclockwise around the low. This inward, cyclonic circulation is the defining pattern around a low in the NH, whereas a high pressure center would produce a clockwise, outward flow.

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