Liu Yang, Koutrakis Petros, Kahn Ralph, Turquety Solene, Yantosca Robert M
Harvard School of Public Health, Boston, MA 02215, USA.
J Air Waste Manag Assoc. 2007 Nov;57(11):1360-9. doi: 10.3155/1047-3289.57.11.1360.
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.
我们使用从多角度成像光谱辐射计(MISR)气溶胶成分测量中得出的分数气溶胶光学厚度(AOD)值,并结合气溶胶传输模型约束条件,来估算美国大陆地区细颗粒物(PM2.5)质量及其主要成分的地面浓度。与美国环境保护局(EPA)现有的地面测量数据相比,使用分数AOD的回归模型能够较好地预测美国东部和西部的PM2.5质量以及硫酸盐(SO4)浓度,还能较好地预测美国西部的硝酸盐(NO3)浓度。与使用总柱AOD作为单一预测因子的类似模型相比,这些模型的预测能力有了显著提高,尤其是在美国西部。这些回归模型中MISR气溶胶成分的相对贡献被用于估算EPA PM2.5物种的粒径分布。该方法捕捉到了美国东部和西部PM2.5质量和SO4颗粒以及西部NO3颗粒粒径分布的整体形状。然而,估算出的PM2.5和SO4模态直径小于之前地面监测研究报告的数值。这可能是由于无法透过云层反演气溶胶导致的卫星采样偏差,以及颗粒物吸湿性对地面测量的粒径分布的影响。