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In a surface low-pressure system, the net inward movement of air occurs due to the pressure gradient force, which drives air from areas of higher pressure toward the lower pressure center. This inflow of air is typically associated with rising air, which leads to the expansion of the air mass. However, as the air rises and cools, it can condense and result in precipitation, ultimately causing the air mass to shrink. This process contributes to the overall dynamics of the low-pressure system, including cloud formation and storm development.

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