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27:. It forms as a result of atmospheric waves caused by wind passing over obstacles; for example, a mountain or a building. They are more common in locations that are hilly, or places where foehn winds are common They tend to look more well-defined when a
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188:"Stratocumulus lenticularis (Sc len) | International Cloud Atlas"
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is causing their formation. They also sometimes show
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cloud type, its appearance is that of a flat lens or
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19:is an uncommon cloud type that belongs to the
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160:. Oxford University Press. p. 87.
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93:Flat stratocumuliform lens or almond
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56:Stratocumulus lenticularis
45:Stratocumulus lenticularis
17:Stratocumulus lenticularis
111:Cirrocumulus lenticularis
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106:Altocumulus lenticularis
154:Whiteman, C.D. (2000).
131:"Stratocumulus clouds"
192:cloudatlas.wmo.int
35:. It is a type of
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37:lenticular cloud
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195:. Retrieved
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171:. Retrieved
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138:. Retrieved
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62:Abbreviation
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33:iridescence
212:Categories
197:2021-11-19
173:2021-11-19
140:2021-11-19
135:Met Office
117:References
90:Appearance
83:500-2000 m
29:foehn wind
100:See also
80:Altitude
65:strt len
223:Stratus
218:Cumulus
164:
25:almond
71:Genus
162:ISBN
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