Aerosol properties vary with the aerosol type, loading, or atmospheric
conditions. We found that a dynamical aerosol model that describes th
e variability of aerosol properties as a function of aerosol optical t
hickness can address this issue. Ambient urban/industrial aerosol is m
easured in the mid-Atlantic region of the United States during the sum
mer of 1993 by automatic Sun/sky radiometers. The volume size distribu
tions inverted from the measured sky radiance represent the entire col
umn of ambient particles. These data depict an aerosol regime in which
accumulation mode particle size and volume increases as optical thick
ness increases. A dynamical aerosol model that is a function of optica
l thickness is constructed by fitting lognormal functions to the volum
e size distributions. It accounts for 60% of the variance in the aeros
ol accumulation mode size distributions. The accumulation mode is repr
esented as a linear combination of two modes: one with volume modal ra
dius 0.11 mu m and the other with modal radius 0.21 mu m. The model is
shown to recreate the correct independently measured sky radiance in
the backscattering direction and to predict the phase function within
model uncertainties of data collected in subsequent years. The model i
s shown to be unbiased with respect to the time of day and to reproduc
e the wavelength dependence measured by the independent Sun measuremen
ts. The dynamic model has substantially different properties than a ''
static'' continental model except for the limited optical thickness ra
nge of 0.0-0.25.