Articles | Volume 26, issue 3
https://doi.org/10.5194/acp-26-2175-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Unveiling the dominant control of the systematic cooling bias in CMIP6 models: quantification and corrective strategies
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- Final revised paper (published on 11 Feb 2026)
- Preprint (discussion started on 12 May 2025)
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-2025-1059', Anonymous Referee #1, 12 May 2025
- AC1: 'Reply on RC1', Jie Zhang, 15 May 2025
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RC2: 'Comment on egusphere-2025-1059', Stephen E. Schwartz, 14 May 2025
- AC2: 'Reply on RC2', Jie Zhang, 05 Jun 2025
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Jie Zhang on behalf of the Authors (11 Jul 2025)
Author's response
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ED: Referee Nomination & Report Request started (14 Jul 2025) by Manish Shrivastava
RR by Stephen E. Schwartz (16 Jul 2025)
RR by Anonymous Referee #1 (21 Jul 2025)
ED: Reconsider after major revisions (17 Aug 2025) by Manish Shrivastava
AR by Jie Zhang on behalf of the Authors (09 Oct 2025)
Author's response
Author's tracked changes
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ED: Referee Nomination & Report Request started (22 Oct 2025) by Manish Shrivastava
ED: Reconsider after major revisions (22 Nov 2025) by Manish Shrivastava
AR by Jie Zhang on behalf of the Authors (31 Dec 2025)
Author's response
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ED: Publish subject to technical corrections (13 Jan 2026) by Manish Shrivastava
AR by Jie Zhang on behalf of the Authors (21 Jan 2026)
Author's response
Manuscript
The manuscript firstly points out that most CMIP6 earth system models (with interactive atmospheric sulfate cycle) present cold biases in the period 1960-1990 (called PHC in the manuscript, pot-hole cooling). The authors performed then a series of investigations searching the relation of this cold bias with sulfate sources and sinks across the available CMIP6 models. The authors finally proposed a single parameter “ESRT”, effective sulfate retention time. This is an interesting diagnostic, relatively stable for a given model and quite useful to characterize its sulfate cycle. It was shown that ESRT has a good capacity to explain the cold bias across models. It is also interesting to see that the authors use the temperature anomalies of the PHC period to “constrain” the optimal value of ESRT. This optimal value is then used to approximate the “right” sulfate deposition rate which is furthermore used in the BCC model with improved performance.
All that said, I have a small concern for what shown in Fig. 1a displaying temperature time series. From those curves, I can deduce that the cold bias of models in the PHC period is not exceptional, not as the authors pointed out, since there is a good trend compared to observation. But the cold bias (at least in the multi-model ensemble mean) occurred before the PHC period, roughly at the point of 1935 where models drift significantly from observation and the cold bias remains for the rest of the time, including the PHC period (1960-1990).