What is associated with convergence at low-pressure systems?

Convergence at low-pressure systems is primarily associated with the upward motion of air. In such systems, air from surrounding areas moves toward the center of the low pressure, creating a convergence zone. As the air converges, it is forced to rise because there is no space for it to remain at the surface. This rising air can lead to the development of clouds and precipitation as it cools, expands, and condenses moisture in the atmosphere.

In contrast, stable atmospheric conditions generally correspond to a lack of significant vertical motion, while air forced downward is characteristic of high-pressure systems, not low-pressure systems. Additionally, wind direction tends to change in response to the pressure systems rather than remaining unchanged, as winds flow from high-pressure areas to low-pressure areas. Thus, the movement of air toward low-pressure regions is inherently linked to creating upward motion in the atmosphere.