What type of currents are present beneath a temperature inversion as described in the context of cloud formation?

The presence of convective currents beneath a temperature inversion is essential for understanding cloud formation dynamics. A temperature inversion occurs when a layer of warmer air traps cooler air near the surface. In this scenario, convection—a process where warmer, less dense air rises and cooler, denser air sinks—can occur only to a limited extent because the warmer air aloft inhibits vertical movement.

The correct answer reflects the situation where there are indeed convective currents present, but these currents are usually moderated due to the stabilization effect of the inversion layer. The presence of moderate winds beneath the temperature inversion allows for some mixing of the air, which can lead to the formation of clouds as humidity rises and condenses.

In contrast, while options mentioning strong winds may accurately describe conditions above the inversion, they don't fully capture the behavior of air currents directly beneath it. The correct choice highlights the moderated nature of these currents, promoting an understanding of how temperature inversions can influence weather patterns and cloud formation on a localized scale.