What phenomena often occur with stratiform clouds?

Stratiform clouds are typically associated with stable atmospheric conditions and widespread, uniform cloud cover. These clouds form in layers and are generally linked to steady, prolonged precipitation rather than intense or convective weather phenomena. The presence of these clouds often indicates a gradual rise in moisture, leading to light to moderate, continuous rain or drizzle, which is why the choice regarding steady precipitation aligns well with the characteristics of stratiform clouds.

Thunderstorms are commonly associated with cumulonimbus clouds, which develop in unstable conditions and are characterized by vertical development, unlike the flatter nature of stratiform clouds. Heavy fog is more often linked to specific humidity and temperature conditions near the ground rather than the overarching characteristics of stratiform clouds. Hail storms typically occur within strong thunderstorms that feature significant updrafts and turbulence, conditions that are not present with the stable stratiform cloud formations. Thus, the relationship between stratiform clouds and steady precipitation makes this choice the most accurate.