2019
DOI: 10.1029/2019gl083673
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An Observation‐Based Correction for Aerosol Effects on Nitrogen Dioxide Column Retrievals Using the Absorbing Aerosol Index

Abstract: Retrievals of nitrogen dioxide (NO2) and other trace gases from satellite measurements rely on accurate calculation of an air mass factor (AMF) to account for the atmospheric light path. Scattering and absorption of sunlight by aerosols affects AMFs by impacting the sensitivity of satellite‐observed radiances to NO2 at different altitudes. Current NO2 retrievals either do not explicitly account for these effects or rely on aerosol information from an external source. Here we investigate a method for quantifyin… Show more

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Cited by 7 publications
(5 citation statements)
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“…Aerosol effects on the scattering weights are not taken into consideration. Based on radiative transfer calculations and satellite-based aerosol products, Y. Jung et al (2019) and Cooper et al (2019) observed small changes (< 10 %) in air mass factors (AMFs) with and without considering the aerosol impacts in Europe in springtime. This tendency likely results from a low aerosol optical depth.…”
Section: Measurements Modeling and Methodsmentioning
confidence: 99%
“…Aerosol effects on the scattering weights are not taken into consideration. Based on radiative transfer calculations and satellite-based aerosol products, Y. Jung et al (2019) and Cooper et al (2019) observed small changes (< 10 %) in air mass factors (AMFs) with and without considering the aerosol impacts in Europe in springtime. This tendency likely results from a low aerosol optical depth.…”
Section: Measurements Modeling and Methodsmentioning
confidence: 99%
“…Aerosols can also contribute to uncertainty in air mass factor calculations, as a reduction in anthropogenic scattering aerosols during lockdowns may reduce air mass factors leading an underestimation of the NO 2 change 62,63 . However, this is likely to be a minor source of uncertainty in estimated NO 2 changes due to lockdown, because aerosol concentration changes were small in most regions 49 and a reduction in aerosol concentration of 10% translates to an uncertainty in NO 2 of less than 5% 64 . Additional uncertainty (σ Ω max ) may arise from the choice of the Ω max parameter (described in the Supplementary Information), particularly in regions where there are insufficient ground-monitor data for constraining Ω max .…”
Section: Limitations and Sources Of Uncertaintymentioning
confidence: 99%
“…Both OMI NO 2 retrievals employed in this study use NO 2 vertical shape factors from coarse resolution simulations, and therefore are biased low compared to in-situ measurements [Goldberg et al, 2017]. These retrievals also have not explicitly accounted for the 400 aerosol optical effects, which are demonstrated to degrade the accuracy of NO 2 column concentrations [Chimot et al, 2016;Liu et al, 2019;Cooper et al, 2019]. The differences in the magnitude of ozone concentrations from GC-adj and GCv12 reflect the impact of other species emissions and chemical mechanisms on the bias of ozone simulations.…”
Section: Discussionmentioning
confidence: 99%