Atmospheric turbidity at athens observatory

Details Atmospheric turbidity at athens observatory Atmospheric turbidity at athens observatory

May 1977

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1977papge.115..583k&link_type=abstract

Pure and Applied Geophysics PAGEOPH, Volume 115, Issue 3, pp.583-591

Physics

Geophysics

Aerosol, Solar Radiation, Turbidity

Scientific paper

In this study, values of the Ångström turbidity coefficient (β) determined from Solar radiation observations at the National Observatory of Athens over the period 1955 1972 are analysed. Mean daily turbidity lies between 0.020 0.100. Turbidity is higher in summer than in winter. The main factor determining the turbidity is the air mass type. The scavenging by rainfall probably has a considerable effect in determining this distribution. There is some evidence of a trend of increasing turbidity during the period.

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