2021
DOI: 10.3390/rs13163163
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Variabilities in PM2.5 and Black Carbon Surface Concentrations Reproduced by Aerosol Optical Properties Estimated by In-Situ Data, Ground Based Remote Sensing and Modeling

Abstract: Because of the increased temporal and spatial resolutions of the sensors onboard recently launched satellites, satellite-based surface aerosol concentration, which is usually estimated from the aerosol optical depth (AOD), is expected to become a strategic tool for air quality studies in the future. By further exploring the relationships of aerosol concentrations and their optical properties using ground observations, the accuracies of these products can be improved. Here, we analyzed collocated observations o… Show more

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Cited by 5 publications
(4 citation statements)
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“…Therefore, as CAMS simulations did not include the Finally, we considered the changes in light-absorbing aerosol in both the boundary layer and the total column. Although this dataset is characterized by high uncertainty (Damiani et al, 2021), the values in 2020 were clearly the lowest on record. The largest relative changes (not shown) occurred before the state of emergency (i.e., in January and February), while the largest absolute change occurred in fall; nonetheless, some reduction was apparent in May.…”
Section: Trends and Seasonal Changesmentioning
confidence: 81%
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“…Therefore, as CAMS simulations did not include the Finally, we considered the changes in light-absorbing aerosol in both the boundary layer and the total column. Although this dataset is characterized by high uncertainty (Damiani et al, 2021), the values in 2020 were clearly the lowest on record. The largest relative changes (not shown) occurred before the state of emergency (i.e., in January and February), while the largest absolute change occurred in fall; nonetheless, some reduction was apparent in May.…”
Section: Trends and Seasonal Changesmentioning
confidence: 81%
“…Light-absorbing aerosols within the boundary layer were estimated to be described in Damiani et al (2021), combining sky radiometer and MAX-DOAS optical property data at UV wavelengths. Then, in the following analysis, we examine the finemode absorbing AOD within the partial column below 1 km (i.e., fAAOD [0-1 km]), which was computed by combining the columnar fine-mode fraction (FMF) and single scattering albedo (SSA) parameters retrieved from the sky radiometer with the mean partial column AOD estimated from MAX-DOAS measurements.…”
Section: Methodsmentioning
confidence: 99%
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