We simulate accumulation of Al2O3 particles in the atmosphere produced by s
olid-fueled rocket motors by using the Goddard Institute for Space Studies/
University of California at Irvine three-dimensional (3-D) chemistry-transp
ort model (CTM). Our study differs from Jackman et al. (1998) by applying a
3-D CTM, considering 13 size bins for the emitted particles from 0.025 to
10 mum and taking into account their washout, gravitational sedimentation,
and coagulation with background sulfate aerosol. We assume an initial trimo
dal size distribution of Al2O3 particles (Beiting, 1997) with 2.8% by mass
of the alumina emitted as particles with radius of less than 1 mum. Our tes
t case adopts a stratospheric source of 1120 tons/yr equivalent to nine spa
ce Shuttle and four Titan IV launches annually. The calculated steady state
surface area density (SAD) and mass density for the scenarios with sedimen
tation of alumina particles have maximum values in the lower stratosphere i
n the Northern Hemisphere of up to 7x10(-4) mum(2)/cm(3) and 0.09 ng/m(3),
respectively, or about 1000 times smaller than those of the background sulf
ate aerosol. Our results are sensitive to the emitted mass fractionation of
alumina (EMFA) showing the values for the SAD or mass density higher or lo
wer by an order of magnitude owing to a poorly known EMFA. Chemical implica
tions of alumina particle accumulation for the ozone balance are estimated
by using the Atmospheric and Environmental Research 2-D model assuming chlo
rine activation on Al2O3 surfaces via the ClONO2 + HCl --> Cl-2 + HNO3 reac
tion with a probability of 0.02 (Molina et al., 1997). Owing to the very sm
all Al2O3 SAD, any additional ozone depletion due to Al2O3 emissions is als
o small (0.0028% on a global annually averaged basis for the scenario with
sedimentation, or about 4 times smaller than the ozone response to chlorine
emissions only). The ozone depletion potential of the alumina emissions is
about 0.03-0.08 for the scenarios using the EMFA of Beiting (1997) and lar
ger by an order of magnitude for the EMFA of Brady and Martin (1995).