Articles | Volume 14, issue 4
https://doi.org/10.5194/amt-14-2857-2021
https://doi.org/10.5194/amt-14-2857-2021
Research article
 | 
13 Apr 2021
Research article |  | 13 Apr 2021

Explicit and consistent aerosol correction for visible wavelength satellite cloud and nitrogen dioxide retrievals based on optical properties from a global aerosol analysis

Alexander Vasilkov, Nickolay Krotkov, Eun-Su Yang, Lok Lamsal, Joanna Joiner, Patricia Castellanos, Zachary Fasnacht, and Robert Spurr

Data sets

OMI/Aura Level 1B VIS Global Geolocated Earth Shine Radiances 1-orbit L2 Swath 13x24 km V003 M. Dobber https://doi.org/10.5067/Aura/OMI/DATA1004

OMI/Aura Global Geometry-Dependent Surface LER 1-Orbit L2 Swath 13x24km V3 J. Joiner, W. Qin, Z. Fasnacht, A. Vasilkov, D. Haffner, B. Fisher, N. Krotkov, L. Lamsal, and R. Spurr https://doi.org/10.5067/AURA/OMI/DATA2032

OMI/Aura Nitrogen Dioxide (NO2) Total and Tropospheric Column 1-orbit L2 Swath 13 × 24 km V003 N. A. Krotkov, L. N. Lamsal, S. V. Marchenko, E. J. Bucsela, W. H. Swartz, J. Joiner, and the OMI core team https://doi.org/10.5067/Aura/OMI/DATA2017

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Short summary
To explicitly account for aerosol effects in the OMI cloud and nitrogen dioxide algorithms, we use a model of aerosol optical properties from a global aerosol assimilation system and radiative transfer computations. Accounting for anisotropic reflection of Earth's surface is an important feature of the approach. Comparisons of the cloud and tropospheric nitrogen dioxide retrievals with implicit and explicit aerosol corrections are carried out for a selected area with high pollution.