Articles | Volume 16, issue 5
https://doi.org/10.5194/esd-16-1739-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.AR6 updates to RF by GHGs and aerosols lowers the probability of accomplishing the Paris Agreement compared to AR5 formulations
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- Final revised paper (published on 16 Oct 2025)
- Supplement to the final revised paper
- Preprint (discussion started on 10 Feb 2025)
- 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-2025-342', Anonymous Referee #1, 31 Mar 2025
- AC2: 'Reply on RC1', Endre Farago, 11 Apr 2025
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RC2: 'Comment on egusphere-2025-342', Anonymous Referee #2, 08 Apr 2025
- AC1: 'Reply on RC2', Endre Farago, 11 Apr 2025
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (29 Apr 2025) by Ben Kravitz

AR by Endre Farago on behalf of the Authors (29 Jun 2025)
Author's response
Author's tracked changes
Manuscript
ED: Referee Nomination & Report Request started (01 Jul 2025) by Ben Kravitz
RR by Anonymous Referee #2 (23 Jul 2025)

RR by Anonymous Referee #3 (28 Jul 2025)

ED: Publish subject to minor revisions (review by editor) (06 Aug 2025) by Ben Kravitz

AR by Endre Farago on behalf of the Authors (14 Aug 2025)
Author's response
Author's tracked changes
Manuscript
ED: Publish as is (15 Aug 2025) by Ben Kravitz
AR by Endre Farago on behalf of the Authors (20 Aug 2025)
Manuscript
Review of AR6 updates to RF by GHGs and aerosols lowers the probability of accomplishing the Paris Agreement compared to AR5 formulations by Farago et al.
Summary
The authors apply an existing multiple linear regression model to decompose the relative contribution of internal and external forcing factors to global mean surface temperature (GMST) change over the 20th and 21st century. They compare the influence of different assumptions about effective radiative forcing from various constituents (but primarily tropospheric aerosols) between two generations of the CMIP protocol (AR5, referred to as Baseline, and AR6). The authors show that their MLR model reproduces the majority of features of the GMST response, and the effective climate sensitivity, simulated by a range of previous simplified and comprehensive modelling efforts. They use this information to provide probabilistic estimates of GMST remaining below Paris targets (1.5C and 2.0C).
Major comments
The paper is well researched, and well written; the figures are clear and communicate the main findings of the analysis. I believe that the conclusions reached are appropriate based on the methods and evidence presented. However, I cannot recommend publication of this manuscript for the following reasons.
First, this reviewer found that the authors have not adequately communicated what are the primary novel contributions of the research. On the contrary, in virtually all cases in the results sections, the authors highlight that their results are consistent with previous studies. This holds true for previous studies using simplified or intermediate-complexity models, and comprehensive modelling like CMIP6. This is a very well-studied field over the past decade, and the authors must articulate clearly how this research advances the discipline beyond what the myriad of previous studies has done.
Second, while the authors must be commended on their attention to detail and the depth of the research undertaken, the manuscript is much too long considering the paucity of new results being presented. At times it felt like a PhD thesis; for example, Section 2.3 provides many textbook-level definitions of ERF for various atmospheric constituents, and Section 2.5 describes every assumption for the inputs of the regression model in intricate detail. This raised the question of who exactly is the target audience for this work? Since the aim is to publish in ESD, there should be an assumption that interested readers will have sufficient background knowledge in climate change science to trust that emissions inventories, sources of natural/internal climate variability etc. are properly referenced and incorporated without the need for such a detailed assessment here. Potentially important and relevant previous literature was also excluded; for example, see: https://iopscience.iop.org/article/10.1088/1748-9326/6/4/044022/meta.
Third, the linear modelling framework itself does not appear to be a new contribution (e.g., McBride et al. 2021). Therefore, it is somewhat surprising that potentially important limitations of the linear model approach are not investigated or advanced in this research. For example, on L513 the authors describe needing to include a third constraint (consistency with recent observed temperature trends) in order to yield solutions that match the GMST time series over the recent past. Given the importance of ERF_CO2 and ERF_AER on the GMST predictions from the EM-GC model, this suggests a probable role for nonlinear interactions between aerosol and CO2 forcing that the current model cannot capture. It would have been interesting to see this commented on, if not addressed, in the research.
Fourth, one of the major findings of the research highlighted by the authors is the apparent increase in warming rate under the AR6 assumptions compared to pre-AR6 (baseline). However, on L502 the authors state that the 6\% higher climate sensitivity in AR6 comes from applying the published formula for ERF_CO2 from AR6 that is larger than the pre-AR6 formula provided by Myhre et al. (1998). Therefore, it appears that the increased warming rate is "baked-in" to the EM-GC model, rather than an emergent property, making the findings of more warming and a lower probability of remaining below the Paris targets largely unsurprising.
Minor comments:
-L23: The overlap of the baseline and AR6 confidence intervals suggests that the statistical evidence for an increase in the mean is rather weak.
-L119 and L122: do the authors mean to say adopted, rather than adapted?
-L152: Can the authors provide the proportions for the different effects in this attribution? Are CO2 concentrations the dominant effect?
-L205: Can the authors comment on why the ERF_AER value changes by so much (15% larger) when the time period is shortened by only 5 years (ending in 2014)?
-L235: This paragraph is very unclear. What is the single best estimate ERF_AER time series? What portion of the difference is highlighted?
-L690: Why did the authors elect to not examine a business-as-usual/ high emission scenario like SSP5-8.5?
-L855: This conclusion is challenging, because the agreement between EM-GC outputs and the observed GMST timeseries is explicitly built in to the EM-GC model, whereas for the majority of CMIP6 models they are freely running through the 20th Century. Whether this reduces the value of those simulations is a matter for debate; perhaps a more nuanced view is that it affects the types of questions that one should ask of the CMIP-class models.