Articles | Volume 19, issue 18
https://doi.org/10.5194/amt-19-5843-2026
https://doi.org/10.5194/amt-19-5843-2026
Research article
 | 
16 Sep 2026
Research article |  | 16 Sep 2026

A multi-angle and polarization-based retrieval algorithm for aerosol layer height of smoke and dust

Pei Li, Yong Xue, Davide Dionisi, Huihui Li, Shuhui Wu, Xingxing Jiang, Botao He, Peng Wang, and Liying Han

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Cited articles

Chen, X., Xu, X., Wang, J., and Diner, D. J.: Can multi-angular polarimetric measurements in the oxygen-A and B bands improve the retrieval of aerosol vertical distribution?, J. Quant. Spectrosc. Ra., 270, 107679, https://doi.org/10.1016/j.jqsrt.2021.107679, 2021a. 
Chen, X., Wang, J., Xu, X., Zhou, M., Zhang, H., Castro Garcia, L., Colarco, P. R., Janz, S. J., Yorks, J., McGill, M., Reid, J. S., de Graaf, M., and Kondragunta, S.: First retrieval of absorbing aerosol height over dark target using TROPOMI oxygen B band: Algorithm development and application for surface particulate matter estimates, Remote Sens. Environ., 265, 112674, https://doi.org/10.1016/j.rse.2021.112674, 2021b. 
Choi, W., Lee, H., Kim, J., and Park, J.: First TROPOMI Retrieval of Aerosol Effective Height Using O4 Absorption Band at 477 nm and Aerosol Classification, IEEE T. Geosci. Remote, 59, 9873–9886, https://doi.org/10.1109/TGRS.2020.3044050, 2021. 
Cohen, J. B., Ng, D. H. L., Lim, A. W. L., and Chua, X. R.: Vertical distribution of aerosols over the Maritime Continent during El Niño, Atmos. Chem. Phys., 18, 7095–7108, https://doi.org/10.5194/acp-18-7095-2018, 2018. 
de Graaf, M., Sneep, M., ter Linden, M., Tilstra, L. G., Donovan, D. P., van Zadelhoff, G.-J., and Veefkind, J. P.: Improvements in aerosol layer height retrievals from TROPOMI oxygen A-band measurements by surface albedo fitting in optimal estimation, Atmos. Meas. Tech., 18, 2553–2571, https://doi.org/10.5194/amt-18-2553-2025, 2025. 
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Short summary
The vertical distribution of aerosols governs their interactions with solar radiation and clouds, making it a key factor in their climatic and environmental effects. Polarization provides independent constraints that reduce ALH (aerosol layer height)–AOD (aerosol optical depth) coupling. A joint optimal estimation method is developed using HARP2 (Hyper-Angular Rainbow Polarimeter-2) observations.
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