Altocumulus cloud
© Kr-val
Altocumulus is a mid-level cloud that usually forms between 6,500 to 22,000 feet. These clouds look partly white and partly greyish, in the form of heaps, rolls or billows. They consist of super-cooled water droplets and often present ice crystals. Usually, this type of cloud doesn’t produce rain but can indicate a change of weather within the day.
On a warm and humid summer morning, altocumulus indicate possible thunderstorms in the late afternoon, or just deterioration in the weather. Some types of altocumulus announce no change in future weather.