Articles | Volume 26, issue 4
https://doi.org/10.5194/acp-26-3025-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
From column to surface: connecting the performance in simulating aerosol optical properties and PM2.5 concentrations in the NASA GEOSCCM
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- Final revised paper (published on 27 Feb 2026)
- Supplement to the final revised paper
- Preprint (discussion started on 26 Jun 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 egusphere-2025-2354', Haihui Zhu, 05 Sep 2025
- RC2: 'Comment on egusphere-2025-2354', Anonymous Referee #2, 30 Sep 2025
- AC1: 'Comment on egusphere-2025-2354', Caterina Mogno, 20 Nov 2025
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Caterina Mogno on behalf of the Authors (20 Nov 2025)
Author's response
Author's tracked changes
Manuscript
ED: Referee Nomination & Report Request started (28 Nov 2025) by Toshihiko Takemura
RR by Anonymous Referee #1 (30 Nov 2025)
RR by Anonymous Referee #2 (18 Dec 2025)
ED: Publish as is (19 Dec 2025) by Toshihiko Takemura
AR by Caterina Mogno on behalf of the Authors (30 Dec 2025)
Manuscript
This study combines longterm AOD observations and detailed ground-based PM2.5 measurements to comprehensively evaluate GEOSCCM performance in surface aerosol, column AOD, and aerosol optical properties. It identifies key factors for improving performance of GEOSCCM and potentially other models. I recommend this manuscript to be published after minor revisions that address questions below.
Specific comments:
L159-160: The ‘Southern Asia’ region is huge and include polluted regions with different behaviors (South Asia vs East Asia). Should justify why they can be combined in this analysis.
Section 4.2:
surface PM2.5 is notably underestimated for most regions except for NA and Aus, despite that AOD is in good agreement with satellite. Could add some discussions about why surface PM tend to be underestimated by GEOSCCM. Are there any previous work on the aerosol vertical distribution that can explain the bias? What could be done in the future for improving the agreement near the surface?
Section 4.3:
(1) the under estimated BC in Figure 6 and good agreement in Figure 7 seem to be suggesting anthropogenic BC not being capture in the model (emission inventory).
(2) There is consistent seasonality bias. And according to IMPROVE, the bias in background dust is getting higher. What could be contributing to this bias and trend? Inland intrusion of dust from the Atlantic Ocean can explain the bias in southeast US and maybe Southern US, but no so much in southwestern US.
Minor comments:
L27: ‘relate more to simulated aerosol mass’ - would be more accurate to say ‘aerosol speciation’
~L300: eqn 1, sigma simple shows up as a question mark in the pdf document.
Table 1: ‘Washington U. S. Louis’ - it is not common to abbreviate ‘St. Louis’ as ‘S. Louis’.
Figure 6: y axis label is cut off for the first and fourth rows.
Table 2: could be moved to the supplements as it is not discussed a lot and figure 8 is illustrative enough.
L484: ‘Dame’ should be ‘Same’
L501: ‘except Europe’ could be removed since the model doesn’t obviously perform worse here.