What distinguishes stratiform clouds from cumuliform clouds?

Stratiform clouds and cumuliform clouds can be distinguished by their structural characteristics. Stratiform clouds are typically flat and layered, forming in sheets that can cover large areas of the sky. These clouds are often associated with stable atmospheric conditions and can lead to steady precipitation. On the other hand, cumuliform clouds have a distinct, puffy appearance, resembling cotton balls or mounds. They form in the presence of rising air and are often indicative of unstable atmospheric conditions, leading to potential thunderstorms and varied weather phenomena.

The classification based on structure is significant for understanding the type of weather conditions that each cloud type may bring. Layered stratiform clouds usually indicate more uniform and drizzle-like precipitation, while the vertical development of cumuliform clouds often results in isolated, short-lived, and sometimes intense convective weather. This understanding is essential for interpreting weather patterns and predicting atmospheric phenomena.