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Stratocumulus cloud
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{{Short description|Family class 3 cloud type}} {{More citations needed|date=September 2008}} {{Infobox Cloud | name = Stratocumulus clouds | image location = Above the Clouds.jpg | image name = Aerial photograph of Stratocumulus perlucidus clouds over the midwestern United States | abbreviation = Sc | symbol =Clouds CL 5.svg | genus = Stratocumulus (layer heap) | species = * Castellanus * Floccus * Lenticularis * Stratiformis * Volutus | variety = * Duplicatus * Lacunosus * Opacus * Perlucidus * Radiatus * Translucidus * Undulatus | altitude_m = 500-2,000 | altitude_ft = 2,000-7,000 | level = low | appearance = Thicker, dark gray, and somewhat conjoined heaps of clouds. | precipitation = Uncommon [[Rain]], [[Snow]] or [[Snow pellets]] | thickness = | Ice content = }} A '''stratocumulus''' [[cloud]], occasionally called a '''cumulostratus''', belongs to a genus-type of clouds characterized by large dark, rounded masses, usually in groups, lines, or waves, the individual elements being larger than those in [[Altocumulus cloud|altocumulus]], and the whole being at a lower height, usually below {{convert|2000|m|ft}}.<ref name="Stratocumulus">{{cite book |editor=World Meteorological Organization |title=Stratocumulus, International Cloud Atlas |volume=I |year=1975 |url=https://archive.org/details/manualonobservat00worl/page/39 |pages=[https://archive.org/details/manualonobservat00worl/page/39 39–42] |isbn=92-63-10407-7 |access-date=28 November 2014 }}</ref><ref>{{cite web|title= International cloud atlas–Definitions of clouds|publisher= [[World Meteorological Organization]]|url= https://cloudatlas.wmo.int/clouds-definitions.html|access-date= 25 September 2018}}</ref> Weak [[Atmospheric convection|convective]] [[air current|currents]] create shallow cloud layers (see also: [[sea of clouds]]) because of drier, stable air above preventing continued vertical development. Historically, in English, this type of cloud has been referred to as a '''twain cloud''' for being a combination of two types of clouds.
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