Articles | Volume 17, issue 8
https://doi.org/10.5194/essd-17-3873-2025
© Author(s) 2025. This work is distributed under the Creative Commons Attribution 4.0 License.
Aerosol single-scattering albedo derived by merging OMI/POLDER satellite products and AERONET ground observations
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- Final revised paper (published on 11 Aug 2025)
- Supplement to the final revised paper
- Preprint (discussion started on 21 Jan 2025)
- Supplement to the preprint
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
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RC1: 'Comment on essd-2024-583', Anonymous Referee #1, 24 Feb 2025
- AC2: 'Reply on RC1', Prof Li, 23 Apr 2025
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RC2: 'Comment on essd-2024-583', Anonymous Referee #2, 26 Mar 2025
- AC1: 'Reply on RC2', Prof Li, 23 Apr 2025
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Jing Li on behalf of the Authors (27 Apr 2025)
Author's response
Author's tracked changes
Manuscript
ED: Referee Nomination & Report Request started (30 Apr 2025) by Jing Wei
RR by Anonymous Referee #2 (21 May 2025)
ED: Publish as is (22 May 2025) by Jing Wei
AR by Jing Li on behalf of the Authors (26 May 2025)
Review comments on “Aerosol single scattering albedo derived by merging OMI/POLDER satellite products and AERONET ground observations” by Dong et al. submitted to the journal Earth System Science Data.
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General comments:
This study by Dong et al. uses Ensemble Kalman Filter (EnKF) data synergy technique to construct Merged-OMI and Merged-POLDER datasets based on SSA products of AERONET, OMI and POLDER. At the same time, the results verify the effectiveness of EnKF technology in extending the information obtained from the ground station to a larger area. The constructed SSA global dataset can provide data support for global aerosol radiative forcing assessment and climate change detection. Overall, this manuscript is clearly written, and the topic is suitable for the journal. I would support for publication in the journal of Earth System Science Data after some corrections and clarifications.
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Specific comments:
Abstract: in order to follow the ESSD requirement, you should mention the generated dataset with register doi in your abstract.
P2 L55: I would draw your attention about two recent and studies related to your discussions by Chen et al. (2020) and Schutgens et al. (2021) about aerosol absorption evaluation and intercomparison between satellite products.
Chen, C., Dubovik, O., Schuster, G.L. et al. Multi-angular polarimetric remote sensing to pinpoint global aerosol absorption and direct radiative forcing. Nat Commun 13, 7459 (2022). https://doi.org/10.1038/s41467-022-35147-y
Schutgens, N., Dubovik, O., Hasekamp, O., Torres, O., Jethva, H., Leonard, P. J. T., Litvinov, P., Redemann, J., Shinozuka, Y., de Leeuw, G., Kinne, S., Popp, T., Schulz, M., and Stier, P.: AEROCOM and AEROSAT AAOD and SSA study – Part 1: Evaluation and intercomparison of satellite measurements, Atmos. Chem. Phys., 21, 6895–6917, https://doi.org/10.5194/acp-21-6895-2021, 2021.
P3 L71: why not merge OMI, POLDER and AERONET into one single global SSA datasets?
P4 L95: could you please explicit how you do average SSA? SSA is a relative value, therefor a direct value average seems meaningless. In addition, SSA is usually provided with certain AOD threshold.
L105: could you please provide proper reference to it?
Section 2.3: if I understood, is it 1D data assimilation? You correct only the grids with ground-based measurements, right?
Line 225: Figure 3 shows that the RMSE of SSA/original-OMI and SSA/AERONET is 0.036, while the RMSE on this figure is 0.035.
Figure 4: there are less effects on Sahara Desert w/wo data assimilation, both Original and Merged-OMI seem underestimate SSA there, could you elaborate more about it?
Figure 6: in most cases/sites, R is improved after merging, while Bias and RMSE could become worse in few sites (6h and 6i), could you explain why is that?
L308: there is a known issue for POLDER measurements at 440 nm.
Section 3.4: since you treat 4 channels (440, 670, 865, and 1020 nm) SSA for POLDER, it would be interesting you check or evaluate the SSA spectral dependence w/wo assimilation.
Figure 17: could you provide the same figure for merged product?