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Nacreous Clouds
(redirected from Polar stratospheric cloud)

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nacreous clouds [′nā·krē·əs ′klau̇dz]
(meteorology)
Clouds of unknown composition, whose form resembles that of cirrus or altocumulus lenticularis, and which show very strong irisation similar to that of mother-of-pearl, especially when the sun is several degrees below the horizon; they occur at heights of about 12 or 18 miles (20 or 30 kilometers). Also known as mother-of-pearl clouds.

Nacreous Clouds 

thin, translucent clouds that occur at high elevations (about 22–30 km). They are observed rather infrequently, usually at latitudes of 55°-60° just before sunrise or just after sunset (against the daytime background of diffused light they are invisible).



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Extreme cold temperatures there produce polar stratospheric clouds.
Potential feedback mechanisms include polar stratospheric clouds (Sloan and Pollard 1998) and hurricane-induced ocean mixing (Emanuel et al.
Key chemical reactions that lead to ozone depletion happen on the surface of rare polar stratospheric clouds (PSCs), which form high up in the atmosphere.
 
 
 
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