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George Kallos, Marina Astitha, Petros Katsafados, and Chris Spyrou

observations, ground-based measurements, and operational modeling forecasts, there is a large seasonal variability of the dust mobilization that depends on the source characteristics as well as the global atmospheric circulation ( di Sarra et al. 2001 ; Ozsoy et al. 2001 ). During winter and spring, the GMR is affected by two upper-air jet streams: the polar-front jet stream, originally located over Europe, and the subtropical jet stream, which is typically located over northern Africa. The combined

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Francis S. Binkowski, Saravanan Arunachalam, Zachariah Adelman, and Joseph P. Pinto

atmospheric aerosol. Atmos. Environ. , 29 , 875 – 883 . Michalsky , J. J. , J. C. Liljegren , and L. C. Harrison , 1995 : A comparison of sun photometer derivations of total column water vapor and ozone to standard measures of same at the Southern Great Plains Atmospheric Radiation Measurement site. J. Geophys. Res. , 100 , 25995 – 26003 . Sander , S. P. , and Coauthors , 2003 : Chemical kinetics and photochemical data for use in atmospheric studies, Evaluation Number 14. NASA Jet

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