DEVELOPMENT AND APPLICATION OF A NEW AIR-POLLUTION MODELING SYSTEM .3. AEROSOL-PHASE SIMULATIONS

Authors
Citation
Mz. Jacobson, DEVELOPMENT AND APPLICATION OF A NEW AIR-POLLUTION MODELING SYSTEM .3. AEROSOL-PHASE SIMULATIONS, Atmospheric environment, 31(4), 1997, pp. 587-608
Citations number
38
Categorie Soggetti
Environmental Sciences","Metereology & Atmospheric Sciences
Journal title
ISSN journal
13522310
Volume
31
Issue
4
Year of publication
1997
Pages
587 - 608
Database
ISI
SICI code
1352-2310(1997)31:4<587:DAAOAN>2.0.ZU;2-G
Abstract
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