An investigation of atmospheric turbidity over Kerkennah Island in Tunisia

Atmospheric turbidity is an important parameter for assessing the air pollution in local areas and controlling the attenuation of solar radiation reaching the Earthʹs surface under cloudless sky. An investigation of atmospheric turbidity has been undertaken in Kerkennah Island (in Tunisia). Turbidity indexes, namely, Linke factor (TL) and Angstrom coefficient (β) were derived directly from measurements taken by pyrheliometer during a year: July (2008) to June (2009). btained from these measurements in this area were compared with measurements performed in a coastal and urban region (Sidi Bou Said) located in the North of Tunisia. A comparison of the seasonal cycle of turbidity at both sites showed: *) maximum values of turbidity in the summer due to dust storms, vertical convection and breeze sea circulation; *) Values of turbidity decrease in the autumn season, due to the decreasing of days of Sirocco and to the increasing of amount of rainfall; *) low values of turbidity index in the winter, due to precipitation removal as well as relative humidity-impacted deposition; *) middle values of turbidity were observed in the spring season. y, diurnal, hourly mean values and frequency of occurrence of the value of each turbidity index were used to characterize variations of atmospheric turbidity. The three-hourly standard meteorological data given by the Meteorological National Institute (Sfax) represent a valuable supplement to the data sets with the pyrheliometer measurements. The analysis of the results shows that there is a high correlation between atmospheric turbidity and local weather conditions, especially temperature and wind speed. The correlation of meteorological parameters (wind speed and temperature) with the turbidity coefficients was analyzed and discussed.