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Aerosol optical thickness monitoring in the mediterranean
Journal of Aerosol Science, 1998The Mediterranean atmosphere is often affected by large plumes of desert dust from Africa or the Middle-East. Although satellite monitoring of the aerosol optical thickness (AOT) is being performed from solar radiances recorded over sea-water (Husar et al.. 1997; Moulin et al., 1998).
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Variations in parameters of aerosol optical thickness in Dushanbe
Izvestiya - Atmospheric and Oceanic Physics, 2014The results of studies of aerosol optical thickness (AOT) in Dushanbe conducted from July 2010 to March 2011 within the AERONET program are discussed. The statistical characteristics of AOT have been shown to significantly vary during dust intrusions. The seasonal variations in the dustiness of the atmosphere have been analyzed.
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Variability of aerosol optical thickness and atmospheric turbidity in Tunisia
Atmospheric Research, 2003The aerosol optical thickness (AOT) τa computed from the spectral sun photometer in Thala (Tunisia) exhibited variability ranging from approximately 0.03 to greater than 2.0 at 870 nm for March–October 2001. These measurements are compared to the aerosol optical thickness computed in Ouagadougou (Burkina-Faso), Banizoumbou (Niger), IMC Oristano ...
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Abstract This work presents the results of investigations of aerosol extinction and aerosol optical thickness in the coastal areas of the southern Baltic Sea. The investigations were carried out under various weather conditions and in various seasons in 1996–2000. Aerosols carried on winds from 300°-N-60° can be regarded as of marine origin.
Tymon Zielinski, A Zielinski
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