Estimating fine particulate matter component concentrations and size distributions using satellite-retrieved fractional aerosol optical depth: part 2--a case study
Liu, Y; Koutrakis, P; Kahn, R; Turquety, S; Yantosca, RM
HERO ID
98197
Reference Type
Journal Article
Year
2007
Language
English
PMID
| HERO ID | 98197 |
|---|---|
| In Press | No |
| Year | 2007 |
| Title | Estimating fine particulate matter component concentrations and size distributions using satellite-retrieved fractional aerosol optical depth: part 2--a case study |
| Authors | Liu, Y; Koutrakis, P; Kahn, R; Turquety, S; Yantosca, RM |
| Journal | Journal of the Air and Waste Management Association |
| Volume | 57 |
| Issue | 11 |
| Page Numbers | 1360-1369 |
| Abstract | We use the fractional aerosol optical depth (AOD) values derived from Multiangle Imaging Spectroradiometer (MISR) aerosol component measurements, along with aerosol transport model constraints, to estimate ground-level concentrations of fine particulate matter (PM2.5) mass and its major constituents in the continental United States. Regression models using fractional AODs predict PM2.5 mass and sulfate (SO4) concentrations in both the eastern and western United States, and nitrate (NO3) concentrations in the western United States reasonably well, compared with the available ground-level U.S. Environment Protection Agency (EPA) measurements. These models show substantially improved predictive power when compared with similar models using total-column AOD as a single predictor, especially in the western United States. The relative contributions of the MISR aerosol components in these regression models are used to estimate size distributions of EPA PM2.5 species. This method captures the overall shapes of the size distributions of PM2.5 mass and SO4 particles in the east and west, and NO3 particles in the west. However, the estimated PM2.5 and SO4 mode diameters are smaller than those previously reported by monitoring studies conducted at ground level. This is likely due to the satellite sampling bias caused by the inability to retrieve aerosols through cloud cover, and the impact of particle hygroscopicity on measured particle size distributions at ground level. |
| Doi | 10.3155/1047-3289.57.11.1360 |
| Pmid | 18069459 |
| Wosid | WOS:000250768400008 |
| Is Certified Translation | No |
| Dupe Override | No |
| Is Public | Yes |
| Language Text | English |
| Is Qa | No |