What is the typical cloud appearance in stable atmospheric conditions?

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In stable atmospheric conditions, the typical cloud appearance is characterized by layers and a flat formation. This occurs because stable air inhibits vertical movement, which leads to the development of stratiform clouds such as stratus or altostratus. These clouds form when moisture in the air condenses horizontally rather than rising to form cumulonimbus clouds, which are often associated with instability and convective activity.

Layers and flat formations are indicative of stable conditions, as they suggest that air is unable to rise significantly. The presence of these clouds can often lead to overcast skies and consistent, gentle precipitation rather than severe weather. In contrast, other cloud types that are combinations of rising air would manifest as fluffy and towering formations or fast-moving and fragmented clouds, which are more common in unstable conditions where convection is at play.

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