Velum is an accessory cloud veil of great horizontal extent, lying close above or attached to the upper part of one or several cumuliform clouds, which often pierce through it. It forms when a moist, stable layer of air is lifted and condenses around growing convective towers, leaving a thin horizontal sheet stretched between or across them. It is distinguished from pileus mainly by its much greater horizontal spread — a long veil rather than a small cap.
Worth knowing
Velum and pileus are close cousins formed by the same lifting, but the WMO separates them purely by scale — velum is a wide veil of great horizontal extent, while pileus is a small cap. Both occur principally with cumulus and cumulonimbus.
Note
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