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altocumulus

[al-toh-kyoo-myuh-luhs]

noun

Meteorology.

plural

altocumulus 
  1. a cloud of a class characterized by globular masses or rolls in layers or patches, the individual elements being larger and darker than those of cirrocumulus and smaller than those of stratocumulus: of medium altitude, about 8000–20,000 feet (2450–6100 meters).



altocumulus

/ ˌæltəʊˈkjuːmjʊləs /

noun

  1. a globular cloud at an intermediate height of about 2400 to 6000 metres (8000 to 20 000 feet)

“Collins English Dictionary — Complete & Unabridged” 2012 Digital Edition © William Collins Sons & Co. Ltd. 1979, 1986 © HarperCollins Publishers 1998, 2000, 2003, 2005, 2006, 2007, 2009, 2012

altocumulus

plural

altocumuli 
  1. A mid-altitude cloud composed of fleecy white or gray patches or bands. Altocumulus clouds generally form between 2,000 and 6,100 m (6,560 and 20,000 ft).

  2. See illustration at cloud

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Word History and Origins

Origin of altocumulus1

First recorded in 1890–95; alto- + cumulus

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