How does air behave in relation to low pressure systems?

In meteorology, low pressure systems are characterized by a region where the atmospheric pressure is lower than that of the surrounding areas. This creates a differential in pressure that influences the movement of air. Air naturally moves from areas of higher pressure to areas of lower pressure in an effort to equalize the pressure differences.

In the context of a low pressure system, air flows inward toward the low pressure center. As air converges toward this area, it is displaced upward, leading to cloud formation and potentially precipitation. This upward motion can also create dynamic weather patterns, such as storms and cyclones, depending on the strength of the low pressure.

The other choices represent behaviors that do not accurately reflect the characteristics of low pressure systems. Air flowing outward would correspond to areas of high pressure, while downward flow typically occurs in high pressure situations as air sinks. Stays stationary would imply no pressure differential exists, which is not the case in a low pressure system. Thus, the correct understanding of air movement in relation to low pressure systems is that it flows inward.