Articles | Volume 26, issue 9
https://doi.org/10.5194/acp-26-5925-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Dissimilar roles of aerosols, nitrogen deposition and ozone on the terrestrial carbon sink in China during 2010–2020
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- Final revised paper (published on 04 May 2026)
- Supplement to the final revised paper
- Preprint (discussion started on 03 Feb 2026)
- Supplement to the preprint
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
| : Report abuse
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RC1: 'Comment on egusphere-2026-16', Anonymous Referee #1, 07 Mar 2026
- AC1: 'Reply on RC1', Nanhong Xie, 30 Mar 2026
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RC2: 'Comment on egusphere-2026-16', Anonymous Referee #2, 11 Mar 2026
- AC2: 'Reply on RC2', Nanhong Xie, 30 Mar 2026
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Nanhong Xie on behalf of the Authors (30 Mar 2026)
Author's response
Author's tracked changes
Manuscript
ED: Referee Nomination & Report Request started (10 Apr 2026) by Jeffrey Geddes
RR by Anonymous Referee #2 (16 Apr 2026)
ED: Publish as is (27 Apr 2026) by Jeffrey Geddes
AR by Nanhong Xie on behalf of the Authors (28 Apr 2026)
Author's response
Manuscript
The manuscript presents a timely and scientifically significant investigation into how China’s "Clean Air Action" has affected the terrestrial carbon cycle. I recommend that this manuscript be accepted subject to minor revisions along the lines below.
1. The manuscript reports many national totals to two decimal places, e.g., 17.93 TgC. Please consider rounding key values more appropriately.
2. The abstract is clear, but the sentence “reversed the dominant atmospheric drivers” is too strong unless supported by a true combined simulation with interactive effects considered. Please reword it.
3. The meaning of “open” in Table 1 should be replaced by more precise wording, such as “enabled” or "on."
4. For the aerosol run, is only aerosol–radiation interaction active, or are aerosol–meteorology feedbacks also active? Please clarify this in Table 1.
5. Could you describe simply how the carbon-nitrogen cycle is treated in the model? For CLM5, the FUN module is developed to simulate plant nitrogen uptake and nitrogen-carbon interactions. What is the difference between your model and FUN?
6. Line 596-597, as both scattering and absorbing aerosols were reduced, the clarification of enhanced scattering is required.
7. NEP is a net result of NPP and heterotrophic respiration. How does the heterotrophic respiration respond to these atmospheric drivers?