Which cloud types would indicate convective turbulence?

Towering cumulus clouds are associated with convective turbulence due to their vertical development and the intense atmospheric processes that create them. These clouds form when warm, moist air rises rapidly, leading to significant vertical currents and associated turbulence. As the air ascends, it cools, condenses, and can form thunderstorms, which are also characterized by powerful updrafts and downdrafts capable of producing turbulent conditions.

The structure of towering cumulus clouds indicates strong lift and active convection. This makes them a clear signal of turbulent conditions in the atmosphere, especially when they develop into cumulonimbus clouds, which bring even more severe weather phenomena.

Other cloud types mentioned, such as stratocumulus, cirrus, and nimbostratus clouds, generally do not exhibit the same level of vertical development or convective activity. Stratocumulus clouds are more stable and often found in layers, cirrus clouds are high-altitude and indicative of fair weather or changing weather patterns but not associated with turbulence, and nimbostratus clouds produce steady precipitation and are characterized by layer formation without the strong turbulence found in convective clouds.