Spatial and temporal variability of the atmospheric turbidity in Tunisia. (November 2016)

• Record Type: Journal Article
• Authors: Saad, Mohamed; Trabelsi, Amel; Masmoudi, Mohamed; Alfaro, Stephane C.
• Is Part Of: Journal of atmospheric and solar-terrestrial physics. Volume 149(2016)
• Page Start: 93
• Page End: 99
• Publication Date: 2016-11
• Subjects: Atmospheric turbidity -- Linke factor -- Angstrom coefficient -- Direct solar radiation; Geophysics -- Periodicals; Atmospheric physics -- Periodicals; Géophysique -- Périodiques; Météorologie physique -- Périodiques; Electronic journals; 551.51
• DOI: 10.1016/j.jastp.2016.10.001
• Languages: English
• ISSNs: 1364-6826

Abstract

Abstract: Atmospheric turbidity is an important parameter in meteorology, climatology and for providing hindsight on particulate air pollution in local areas. In this work we exploit 1260 direct solar radiation measurements performed in Sfax (Center Tunisia), from March 2015 to February 2016. These measurements were made with a pyrheliometer only when clouds did not obstruct the solar disk. The atmospheric turbidity is quantified by the means of both the Linke's turbidity factor ( T LI ) and Angström's coefficient ( β ). Over the year, values of T LI and β are found to vary in the ranges 1–15 and 0–0.7, with the most probable values around 3.5 and 0.05, respectively. However, a marked seasonal pattern is observed for the two turbidity parameters. They achieve their maximum in the spring and summer months, their minimum in winter and autumn appears as a transitional period. The comparison of the results obtained in Sfax with those of three AERONET stations located in north (Carthage), central-north (Ben Salem), and south (Medenine) Tunisia, reveals that this seasonal pattern of the atmospheric turbidity is valid for all the Tunisian territory, and probably beyond. At shorter (hourly) time scales, the diurnal behavior of the turbidity in Sfax is different in the summer months from the one observed during the rest of the year. Indeed, an enhancement of T LI is observed during the day. This is assumedly attributed to the production of secondary aerosols by atmospheric photochemistry. Highlights: Atmospheric turbidity is measured at 4 Tunisian sites. Its seasonal variability is the same at all sites. Maxima are achieved in spring and minima in winter.