What is one consequence of a strong pressure gradient?

A strong pressure gradient leads to a rapid change in atmospheric pressure over a short distance, which is a primary driver of wind in the atmosphere. When the pressure difference is significant, it results in stronger winds as the air attempts to move from areas of high pressure to low pressure. This movement of air can contribute to turbulence and instability within the atmosphere, creating conditions that are conducive to storm development.

Furthermore, when there are strong winds associated with a steep pressure gradient, they can enhance existing weather systems or contribute to the formation of new ones, such as thunderstorms, particularly when combined with moisture and instability in the atmosphere. Thus, the relationship between a strong pressure gradient and storm development is well established in meteorology.

This reasoning clarifies why the increased likelihood of storms is the correct consequence of a strong pressure gradient. The other options do not align with the established effects of pressure gradients in the atmosphere.