Atmospheric Chemistry and Physics www.atmos-chem-phys.net 1680-7316 1680-7324 3 6 2003 10.5194/acp-3-1903-2003 http://www.atmos-chem-phys.net/3/1903/2003/ http://www.atmos-chem-phys.net/3/1903/2003/acp-3-1903-2003.html http://www.atmos-chem-phys.net/3/1903/2003/acp-3-1903-2003.pdf 1903 1917 2003-11-03 Characteristics and direct radiative effect of mid-latitude continental aerosols: the ARM case M. G. Iziomon U. Lohmann Department of Physics and Atmospheric Science, Dalhousie University, Halifax, Canada A multi-year field measurement analysis of the characteristics and direct radiative effect of aerosols at the Southern Great Plains (SGP) central facility of the Atmospheric Radiation Measurement (ARM) Program is presented. Inter-annual mean and standard deviation of submicrometer scattering fraction (at 550 nm) and Ångström exponent å (450 nm, 700 nm) at the mid-latitude continental site are indicative of the scattering dominance of fine mode aerosol particles, being 0.84±0.03 and 2.25±0.09, respectively. We attribute the diurnal variation of submicron aerosol concentration to coagulation, photochemistry and the evolution of the boundary layer. Precipitation does not seem to play a role in the observed afternoon maximum in aerosol concentration. Submicron aerosol mass at the site peaks in the summer (12.1±6.7<font face="Symbol">m</font>g m^-3), with the summer value being twice that in the winter. Of the chemically analyzed ionic components (which exclude carbonaceous aerosols), SO₄⁼ and NH₄⁺ constitute the dominant species at the SGP seasonally, contributing 23-30% and 9-12% of the submicron aerosol mass, respectively. Although a minor species, there is a notable rise in NO₃^- mass fraction in winter. We contrast the optical properties of dust and smoke haze. The single scattering albedo <font face="Symbol">w</font>₀ shows the most remarkable distinction between the two aerosol constituents. We also present aircraft measurements of vertical profiles of aerosol optical properties at the site. Annually, the lowest 1.2 km contributes 70% to the column total light scattering coefficient. Column-averaged and surface annual mean values of hemispheric backscatter fraction (at 550 nm), <font face="Symbol">w</font>₀ (at 550 nm) and å (450 nm, 700 nm) agree to within 5% in 2001. Aerosols produce a net cooling (most pronounced in the spring) at the ARM site