Mz. Jacobson, DEVELOPMENT AND APPLICATION OF A NEW AIR-POLLUTION MODELING SYSTEM .3. AEROSOL-PHASE SIMULATIONS, Atmospheric environment, 31(4), 1997, pp. 587-608
Result from a new air pollution model were tested against data from th
e Southern California Air Quality Study (SCAQS) period of 26-29 August
1987. Gross errors for sulfate, sodium, light absorption, temperature
s, surface solar radiation, sulfur dioxide gas, formaldehyde gas, and
ozone were lowest among parameters compared (1-40%). Gross errors for
elemental carbon, organic carbon, total particulate mass, ammonium, am
monia gas, nitric acid gas, and light scattering, were larger (40-61%)
. Gross errors for particulate nitrate were largest (65-70%). Reducing
the baseline land-based particulate emissions inventory to one-third
its original value did not affect gross errors significantly; however,
it did turn overpredictions into underpredictions for many species. D
oubling emissions increased gross errors for nearly all parameters. Se
tting lateral boundary inflow concentrations of particles to zero caus
ed slight (<1%) erosion of results for most species, large erosion (10
%) for sodium and chloride, but slight improvement (<1%) for a few spe
cies. Setting both lateral inflow and initial concentrations for gases
and particles to zero caused severe degradation of results for many s
pecies but relatively mild degradation or improvement for a few. Spinn
ing up the meterological model 24 h in advance caused most gross error
s to increase. Finally, the presence of aerosols reduced peak daytime
surface solar radiation by approximately 6.4% (55 W m(-2)), increased
nighttime temperatures by about 0.77 K, decreased daytime temperatures
by about 0.08 K, and increased overall temperatures (day plus night)
by 0.43 K compared to a no-aerosol case. The presence of aerosols also
caused ozone mixing ratios to decrease by 2%. Copyright (C) 1996 Else
vier Science Ltd