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References:
Wang, J., and S.A. Christopher, Intercomparison between satellite-derived aerosol optical thickness and PM2.5 mass: Implication for air quality studies, Geophys. Res. Lett., 108 (21), doi:10.1029/2003GL018174, 2003. (pdf file)
Christopher, S. A. and J. Wang, 2003: Exploring the Potential of Satellite Data for Air Quality Applications, Eos Trans. AGU, 84(46), Fall Meet. Suppl., Abstract A11E-0033, 2003. (pdf file, download first and then open it)
1. Introduction
Particular matters, or aerosols, reduce visibility, affect human health, and
also cause several ecological effects. As defined by Environment Protection
Agency (EPA), the dry mass content of particular matter with aerodynamic
diameter less than 2.5 µm (PM2.5) in the atmosphere is an important parameter
for the evaluation of air quality. However, the large spatiotemporal variations
of particular matter make it a challenge to judge the air quality and issue
prompt health alert from the current ground-based measurement network,
especially when the aerosol events come from sources outside the U.S. The launch
of EOS TERRA and AQUA satellite provides an unprecedented opportunity to monitor
the air pollution over the globe. The intent of this study is to explore the
potential of satellite aerosol datasets for air quality applications.
2. Hypothesis and Methodology
Aerosols with diameters around 1 ~2µm are efficient in scattering the visible
light. During MODIS passing time (locally, 10:30AM for TERRA and 1:30 for AQUA)
in clear sky conditions, the atmospheric boundary layer is well mixed. Hence,
the MODIS visible reflectance and its column aerosol optical thickness (AOT)
retrievals can be used as indicators of the PM2.5 mass at the surface. In this
study, we compared MODIS AOT with the ground-based PM2.5 hourly measurements.
For each comparison, MODIS AOT time is centered around the PM2.5 observation
time period. The final goal of this comparison is to evaluate the quality of
MODIS AOTs in the context of air quality applications before they are
assimilated into the air quality models. This is important because
evaluation of data quality is a critical step in the data assimilation
processes.
3. Data and Study Area
4. A Case Demo. (more cases and analysis can be found in our paper and poster)
| The following figures show a heavy haze event identified by the spatial distribution of MODIS AOT. Also shown is the linearly derived Air Quality Index (AQI) and the 700mb geopotential heights. Grey regions are areas where MODIS AOT is not available due to possible sun glint or cloud contamination. |
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5. Conclusions
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Copyright © 2009 Dr. Jun Wang, Geosciences, University of Nebraska-Lincoln