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t h e air, are calculated, on the basis of continuous recording wich are carried
out in the central adriatic region, using Gerdien cylindrical condensers,
during the years 1970/1974.
Dissimilarities between thundersthorms, fogs and foelin winds are
evaluated, together with the hourly behavior of the dust, which result
greatly antiparallel to t h e behavior of t h e electrical conductivity of the air.
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