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Stratocumulus cloud
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== Formation == Stratocumulus clouds usually form from the rising and breakup of a [[stratus cloud]].<ref name="metoffice" /><ref name="ICA-SC-Formation">{{harvnb|Cohn|Bruhn|Anderson|Atkinson|2017|loc=Section 2.3.7.5}}</ref> They can also form from [[altostratus cloud|altostratus]] and [[nimbostratus cloud]]s, either as evaporating precipitation condenses into a cloud or as the nimbostratus cloud itself thins and breaks up. If a cumulus cloud becomes flattened (for example, by [[wind shear]] or [[temperature inversion]]), it too can become a stratocumulus cloud.<ref name="ICA-SC-Formation" />
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