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Quantification of the atmospheric<br />
aerosol content is mandatory<br />
here another example<br />
Falchi, Cinzano 2006, in prep.<br />
45 deg elevation<br />
local<br />
45 deg elevation<br />
local<br />
45 deg elevation, data after h24<br />
cleanest nights 2003-2005,<br />
zenith<br />
snow