The laboratory results may be related to the behaviour of marinestratocumulusclouds.
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The stability ofstratocumulusclouds with strong evaporative cooling effects is explored in laboratory simulations.
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Drizzle is normally produced by low stratiform clouds andstratocumulusclouds.
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Like all other forms ofstratocumulusapart from castellanus, they are also often found in anticyclones.
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This often does not apply whenstratocumulusis of a broken, fractus form, when it may appear as small as altocumulus.
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Stratocumuluscastellanus may develop into cumulus congestus (and even further into cumulonimbus) under auspicious conditions.
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They are distinct from otherstratocumulusby puffy tower-like formations atop the cloud layer.
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The low, sharp temperature inversion can lead to areas of persistentstratocumulusor stratus cloud, known in colloquial terms as anticyclonic gloom.
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Vast areas of subtropical and polar oceans are covered with massive sheets ofstratocumulus.
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This can create the illusion of continuous precipitation of more than very light intensity falling fromstratocumulus.
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Stratocumulusclouds are the main type of cloud that can produce crepuscular rays.
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The levels of albedo present in the low-level marinestratocumulusclouds create a significant global cooling effect.
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The two genera that are strictly low-tage are stratus, andstratocumulus.
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The low, sharp inversion can lead to areas of persistentstratocumulusor stratus cloud, colloquially known as anticyclonic gloom.
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Additionally,stratocumulusclouds reflect a large amount of the incoming sunlight, producing a net cooling effect.
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