Assessing uncertainties of a geophysical approach to estimate surface fine particulate matter distributions from satellite-observed aerosol optical depth

<p>Health impact analyses are increasingly tapping the broad spatial coverage of satellite aerosol optical depth (AOD) products to estimate human exposure to fine particulate matter (PM<span class="inline-formula"><sub>2.5</sub></span>). We use a forward geoph...

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Bibliographic Details
Main Authors: X. Jin, A. M. Fiore, G. Curci, A. Lyapustin, K. Civerolo, M. Ku, A. van Donkelaar, R. V. Martin
Format: Article
Language:English
Published: Copernicus Publications 2019-01-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/19/295/2019/acp-19-295-2019.pdf
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Summary:<p>Health impact analyses are increasingly tapping the broad spatial coverage of satellite aerosol optical depth (AOD) products to estimate human exposure to fine particulate matter (PM<span class="inline-formula"><sub>2.5</sub></span>). We use a forward geophysical approach to derive ground-level PM<span class="inline-formula"><sub>2.5</sub></span> distributions from satellite AOD at 1&thinsp;km<span class="inline-formula"><sup>2</sup></span> resolution for 2011 over the northeastern US by applying relationships between surface PM<span class="inline-formula"><sub>2.5</sub></span> and column AOD (calculated offline from speciated mass distributions) from a regional air quality model (CMAQ; <span class="inline-formula">12×12</span>&thinsp;km<span class="inline-formula"><sup>2</sup></span> horizontal resolution). Seasonal average satellite-derived PM<span class="inline-formula"><sub>2.5</sub></span> reveals more spatial detail and best captures observed surface PM<span class="inline-formula"><sub>2.5</sub></span> levels during summer. At the daily scale, however, satellite-derived PM<span class="inline-formula"><sub>2.5</sub></span> is not only subject to measurement uncertainties from satellite instruments, but more importantly to uncertainties in the relationship between surface PM<span class="inline-formula"><sub>2.5</sub></span> and column AOD. Using 11 ground-based AOD measurements within 10&thinsp;km of surface PM<span class="inline-formula"><sub>2.5</sub></span> monitors, we show that uncertainties in modeled PM<span class="inline-formula"><sub>2.5</sub>∕AOD</span> can explain more than 70&thinsp;% of the spatial and temporal variance in the total uncertainty in daily satellite-derived PM<span class="inline-formula"><sub>2.5</sub></span> evaluated at PM<span class="inline-formula"><sub>2.5</sub></span> monitors. This finding implies that a successful geophysical approach to deriving daily PM<span class="inline-formula"><sub>2.5</sub></span> from satellite AOD requires model skill at capturing day-to-day variations in PM<span class="inline-formula"><sub>2.5</sub>∕AOD</span> relationships. Overall, we estimate that uncertainties in the modeled PM<span class="inline-formula"><sub>2.5</sub>∕AOD</span> lead to an error of 11&thinsp;<span class="inline-formula">µ</span>g&thinsp;m<span class="inline-formula"><sup>−3</sup></span> in daily satellite-derived PM<span class="inline-formula"><sub>2.5</sub></span>, and uncertainties in satellite AOD lead to an error of 8&thinsp;<span class="inline-formula">µ</span>g&thinsp;m<span class="inline-formula"><sup>−3</sup></span>. Using multi-platform ground, airborne, and radiosonde measurements, we show that uncertainties of modeled PM<span class="inline-formula"><sub>2.5</sub>∕AOD</span> are mainly driven by model uncertainties in aerosol column mass and speciation, while model representation of relative humidity and aerosol vertical profile shape contributes some systematic biases. The parameterization of aerosol optical properties, which determines the mass extinction efficiency, also contributes to random uncertainty, with the size distribution being the largest source of uncertainty and hygroscopicity of inorganic salt the second largest. Future efforts to reduce uncertainty in geophysical approaches to derive surface PM<span class="inline-formula"><sub>2.5</sub></span> from satellite AOD would thus benefit from improving model representation of aerosol vertical distribution and aerosol optical properties, to narrow uncertainty in satellite-derived PM<span class="inline-formula"><sub>2.5</sub></span>.</p>
ISSN:1680-7316
1680-7324