Ja. Al-saadi et al., Response of middle atmosphere chemistry and dynamics to volcanically elevated sulfate aerosol: Three-dimensional coupled model simulations, J GEO RES-A, 106(D21), 2001, pp. 27255-27275
The NASA Langley Research Center Interactive Modeling Project for Atmospher
ic Chemistry and Transport (IMPACT) model has been used to examine the resp
onse of the middle atmosphere to a large tropical stratospheric injection o
f sulfate aerosol, such as that following the June 1991 eruption of Mount P
inatubo. The influence of elevated aerosol on heterogeneous chemical proces
sing was simulated using a three-dimensional climatology of surface area de
nsity (SAD) developed using observations made from the Halogen Occultation
Experiment, Stratospheric Aerosol and Gas Experiment II, and Stratospheric
Aerosol Measurement satellite instruments beginning in June 1991. Radiative
effects of the elevated aerosol were represented by monthly mean zonally a
veraged heating perturbations obtained from a study conducted with the Euro
pean Center/Hamburg (ECHAM4) general circulation model combined with an obs
ervationally derived set of aerosol parameters. Two elevated-aerosol simula
tions were integrated for 3 1/2 years following the volcanic injection. One
simulation included only the aerosol radiative perturbation, and one simul
ation included both the radiative perturbation and the elevated SAD. These
perturbation simulations are compared with multiple-year control simulation
s to isolate relative contributions of transport and heterogeneous chemical
processing. Significance of modeled responses is assessed through comparis
on with interannual variability. Dynamical and photochemical contributions
to ozone decreases are of comparable magnitude. Important stratospheric che
mical/dynamical feedback effects are shown, as ozone reductions modulate ae
rosol-induced heating by up to 10% in the lower stratosphere and 25% in the
middle stratosphere. Dynamically induced changes in chemical constituents
which propagate into the upper stratosphere are still pronounced at the end
of the simulations.