Scud clouds are low, detached, irregular clouds that are often seen beneath nimbostratus clouds. They typically appear as low, ragged fragments or patches, and are often dark grey in color. Scud clouds are often associated with rain showers or thunderstorms, as they form in the turbulent air near the base of these storm clouds.
Scud clouds are not true cloud types but rather a type of cloud feature that forms in response to atmospheric turbulence. They are typically short-lived and can change shape rapidly as they are moved by the wind. Scud clouds are commonly seen in unstable atmospheric conditions and are often an indicator of unsettled weather.
Overall, scud clouds are not typically considered to be a significant weather threat, but they can be indicative of atmospheric instability and the potential for stormy weather to come.
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