the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
| 19 Feb 2024
Bringing it all together: Science and modelling priorities to support international climate policy
Abstract. We review how the international modelling community, encompassing Integrated Assessment models, global and regional Earth system and climate models, and impact models, have worked together over the past few decades, to advance understanding of Earth system change and its impacts on society and the environment, and support international climate policy. We then recommend a number of priority research areas for the coming ~6 years (i.e. until ~2030), a timescale that matches a number of newly starting international modelling activities and encompasses the IPCC 7th Assessment Report (AR7) and the 2nd UNFCCC Global Stocktake. Progress in these areas will significantly advance our understanding of Earth system change and its impacts and increase the quality and utility of science support to climate policy.
We emphasize the need for continued improvement in our understanding of, and ability to simulate, the coupled Earth system and the impacts of Earth system change. There is an urgent need to investigate plausible pathways and emission scenarios that realize the Paris Climate Targets, including pathways that overshoot the 1.5 °C and 2 °C targets, before later returning to them. Earth System models (ESMs) need to be capable of thoroughly assessing such warming overshoots, in particular, the efficacy of negative CO2 emission actions in reducing atmospheric CO2 and driving global cooling. An improved assessment of the long-term consequences of stabilizing climate at 1.5 °C or 2 °C above pre-industrial temperatures is also required. We recommend ESMs run overshoot scenarios in CO2-emission mode, to more fully represent coupled climate - carbon cycle feedbacks. Regional downscaling and impact models should also use forcing data from these simulations, so impact and regional climate projections are as realistic as possible. An accurate simulation of the observed record remains a key requirement of models, as does accurate simulation of key metrics, such as the Effective Climate Sensitivity. For adaptation, improved guidance on potential changes in climate extremes and the modes of variability these extremes develop in, is a key demand. Such improvements will most likely be realized through a combination of increased model resolution and improvement of key parameterizations. We propose a deeper collaboration across modelling efforts targeting increased process realism and coupling, enhanced model resolution, parameterization improvement, and data-driven Machine Learning methods.
With respect to sampling future uncertainty, increased collaboration between approaches that emphasize large model ensembles and those focussed on statistical emulation is required. We recommend increased attention is paid to High Impact Low Likelihood (HILL) outcomes. In particular, the risk and consequences of exceeding critical tipping points during a warming overshoot. For a comprehensive assessment of the impacts of Earth system change, including impacts arising directly from specific mitigation actions, it is important detailed, disaggregated information from the Integrated Assessment Models (IAMs) used to generate future scenarios is available to impact models. Conversely, methods need to be developed to incorporate potential future societal responses to the impacts of Earth system change into scenario development.
Finally, the new models, simulations, data, and scientific advances, proposed in this article will not be possible without long-term development and maintenance of a robust, globally connected infrastructure ecosystem. This system must be easily accessible and useable across all modelling communities and across the world, allowing the global research community to be fully engaged in developing and delivering new scientific knowledge to support international climate policy.
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CC1: 'Comment on egusphere-2024-453 (Bjorn Stevens)', Bjorn Stevens, 26 Feb 2024
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2024/egusphere-2024-453/egusphere-2024-453-CC1-supplement.pdf
- CC2: 'Comment on egusphere-2024-453', Rasmus Benestad, 27 Feb 2024
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RC1: 'Comment on egusphere-2024-453', Anonymous Referee #1, 05 Apr 2024
Review of the paper “Bringing it all together: Science and modeling priorities to support international climate policy”, by Jones C.G. et al.
Overview
The paper considers international climate policy needs for science and modeling out to 2030, and lays out priorities across seven areas. These range from modeling coordination in support of the assessment reports (AR) of the Intergovernmental Panel for Climate Change (IPCC), to underpinning science foci, and also the required technological infrastructure. The paper is penned by a large team of European authors involved in IPCC, the Coupled Model Intercomparison Project (CMIP) and more generally the climate science and modeling enterprise.
The focus of the paper is important. As climate change aggravates, and the stakes for climate science and policy get higher, it is critical to have clear climate science and modeling priorities, and community coordination around those, to rapidly accelerate progress. The paper is also timely, as CMIP7 and IPCC AR7 are getting underway. The commentary adds the viewpoint of a segment of the European modeling community, to a number of manuscripts on modeling strategy that have been recently been published or circulated across the international modeling community.
The priorities outlined in the paper are a reasonable evolution of what’s already at play, and aim at addressing some current gaps. Overall, this Reviewer agrees with the points made in this article.
A number of specific major comments/recommendations are listed below, along with some minor points.
Overall the paper is well-written and a useful contribution to on-going community discussions around the future of climate modeling and underpinning science.
Major Points
Line 180. The type of infrastructure outlined here still reflects a linear model from modeling to services, whereby the modeling community decides what simulations to run and shares those with users. Given the rapidly evolving climate policy questions, we should prioritize the development of an infrastructure that supports co-production of information based on climate models (i.e., experiments that are responsive to the evolving needs); that supports ML/AI exploitation of both modeling data and observations to address service needs in a flexible manner.
Lines 240-280. Indeed, the lack of consistency and disconnects in modeling across IPCC WG1-WG2-WG3, and the relevant modeling frameworks (CMIP/CORDEX/IAMS, etc.) are major gaps that need to be addressed. The authors do a great job of explaining current shortcomings and what could be done to address them. In the recommendations (lines 270-280), it seems important to emphasize that: 1) continuing CMIP experiments is critical to the continued improvement of models and scientific understanding; 2) a common framework of protocols, forcings, evaluation metrics, etc. is necessary across the various modeling communities to address the disconnects (e.g., between CMIP and CORDEX); common workflows are necessary but not sufficient; 3) the recommended service oriented/quasi-operational activity and CMIP/CORDEX science activities should be well-connected, i.e. the service activity (from global to local scales) should be a purposeful spin-off of the CMIP, and service needs should be driving CMIP science.
Lines 285-300. This is a great set of questions to illustrate the climate/Earth system modeling needs to inform climate mitigation. It is increasingly clear that changes in aerosols are a critical factor in the Earth’s energy budget and that future mitigation pathways need to consider aerosol/air quality policies. Hence, I recommend explicitly mentioning a question about understanding the interplay of GHGs and aerosols in determining future climate mitigation pathways.
Lines 305-315. In addition to carbon interventions through AFOLU, there are many other types of carbon dioxide removal (CDR) methodologies that are being proposed, including enhancing the ocean carbon uptake (mCDR). Hence, ESM should also capture relevant ocean carbon cycle processes not just land CDR processes. I recommend the discussion be amended in this regard.
Lines 350-370. This is a great list of Earth system interactions to be examined. I would add “humans-climate/ES interactions” to this list, as humans are the current major driver of change at this point. Given the discussions regarding intentional climate interventions, as we learn about how air quality policies are affecting climate, as we are looking to diverse solutions to the climate, biodiversity and socio-economic crises, it becomes increasingly important to factor in humans in ways that are more advanced than what we have thus far. I would recommend the authors make an additional effort in this regard across the paper.
Lines 375-390. The focus of this section on improving regional climate information is appreciated, however the discussion could be improved in several respects. 1) Global variable resolution models and two-way nested global models, both achieving resolutions comparable to regional climate models, are now a reality. These should be mentioned along side more traditional regional climate models. 2) The paper mentions models “..all running in a tightly linked framework..”. Indeed, this simulation workflow is needed. What’s also needed but not mentioned, is a common, model-agnostic, evaluation framework, with metrics and standards applicable across various modeling methodologies; this is increasingly important as the types of modeling methodologies diversify, e.g. with the advent of AI-based models. 3) It is striking that ML/AI is not mentioned in this discussion. It is certainly a promising tool e.g., to get to higher resolution information from lower resolution models, again duly vetted as any other modeling tool.
Line 450. This is a good description of the opportunity provided by CMIP7 to explore using higher resolution in a balanced way, considering also other important lines of research. What I see missing, is an explicit discussion of the value of model diversity, as we try to gauge uncertainty. If we had a perfect way to model climate processes, we could forgo that. But there are still significant uncertainties and errors and so model diversity continues to be crucial.
Lines 470-480. I generally agree with the recommendation of creating a tighter linkage between the global climate modeling (CMIP) and regional modeling (CORDEX). However, we now have global models that can get to convective-scale resolutions at the regional level, via 2-way nesting and variable resolution. These types of models would inherently bring more consistency across spatial scales and could naturally allow for a convergence of the global and regional modeling communities. Some additional discussion of these diverse opportunities is necessary here.
Lines 520-535 A few considerations: 1) “Digital Twins of the Earth” (DTE) are, thus far, primarily focused on atmospheric dynamics rather than Earth system modeling; 2) The value of DTE for climate modeling will need to be evaluated with the same frameworks/metrics that we use for any new modeling tools; this value remains to be proven; 3) DTE for climate will need to explore uncertainties (modeling/data choices, internal variability, forcings, etc.); this is a “must” for any application to climate risk evaluation, as discussed in section 7; 4) it is not unique to DTE to attain km-scale resolution and be responsive to user needs. Global-convection resolving models and variable high-res climate models are a reality. The discussion of DTE should touch on all these points, to illustrate how DTE is an interesting concept but its application to climate modeling is quite aspirational at this point.
Lines 750-795. This is a very well-written description of the status of the modeling infrastructure and the gaps that need to be addressed. One point that seems worth emphasizing: we need to evolve to an infrastructure that allows greater co-production of information between the modeling centers and the users, and greater flexibility.
Section 9. A few things seem worth addressing here and throughout the paper: 1) Climate policy requires that we project out at least 100 years from the present time. It is critically important that CMIP7/AR7 cover at least the period until 2130. 2) Aerosols should be mentioned explicitly as something that we need to study in conjunction with changes in the carbon budget, as we examine future climate mitigation pathways. 3) It is notable that the paper does not touch on modeling of solar radiation modification. As these types of intervention/geoengineering are being proposed, it seems important to document potential impacts and uncertainties. 4) The paper does a good job of discussing the importance of quantifying uncertainty and how it flows across modeling systems. However, the importance of understanding predictability (what we think we can predict and why) is not explicitly addressed. 5) Lastly, the recommendation to be more inclusive of global South scientists is meritorious and could be even more convincing if the paper were to include views from co-authors from that region.
Minor Points
Abstract. It seems important to add an upfront qualifier, that this is a perspective from a group of European authors.
Line 75. The stated time horizon for the priorities outlined in the paper is 6 years, out to 2030. Given what is outlined, this does not seem realistic given the inertia in the enterprise and also the type of recommendations that are provided. We understand the desire to be relevant to the CMIP7/AR7 cycle but it would be more realistic to talk about a 10-year time horizon.
Figure 1. This figure could be improved so that it is readily understandable. The boxes could identify the primary function in plain language and add the acronym in smaller font, e.g. “Global Coupled Modeling – CMIP”, “Regional Climate Modeling - CORDEX”, etc.
Throughout the paper, acronyms should be spelled out. For instance, in lines 540, 585 what are EffCS, TCR, TCRE?
Line 450. “..and for supporting climate change adaptation.” Such references should be amended throughout the paper to also include mitigation, where it is applicable.
Line 590. “For RCMS too short evaluation runs..” This is another place to iterate the need for a common protocol/evaluation framework for regional scale modeling, agnostic of the modeling tool, whether it is a GCM, RCM or an AI based model.
Citation: https://doi.org/10.5194/egusphere-2024-453-RC1 -
RC2: 'Comment on egusphere-2024-453', Anonymous Referee #2, 06 Apr 2024
Review of “Bringing it all together: Science and modeling priorities to support international climate policy” by Jones et al.
The manuscript is an opinion article presenting a large number of authors’ views on the (past and) present state of the international Earth system / climate modeling efforts, including assessment, impact, regional, etc. modeling and their recommendations on a number of priority research areas moving forward. As such, it will be another addition to the recent surge of similar opinion articles (some cited already in the manuscript). While I will respect the authors’ opinions in my review because of the nature of the manuscript, I will offer a few comments and suggestions for authors’ consideration below.
- As I indicated above, there has been a recent surge of similar opinion pieces which advocate for similar approaches going forward based on lessons learnt from the previous related efforts. The current effort is certainly more comprehensive than the others, but it will be useful to mention these recent reviews / opinions up front to provide the context and the need for the present manuscript, essentially answering why the community needs another such piece.
- As far as I can tell, all the co-authors of this manuscript are from European institutions. So, this article represents ONLY a “European” view of how these truly international – not just European – efforts need to be done. International community is not just Europe! This should be made clear.
- The title may be interpreted to imply that the community does Earth system and climate modeling in service to climate policy only. I do not think that this is the intention of the authors. It is important to clarify that Earth system science stands on its own and a subset of related efforts serve the international climate policy.
- We are in the era of co-development, co-design, co-planning, co-analysis, co-etc. of all these efforts with the communities that are impacted by climate change. While the article mentions mitigation, adaptation, etc. and related efforts, given the author list, all of these views and recommendations do not really reflect the views of impacted communities and the Global South for that matter. To avoid “we know the best for your community” perception, please be mindful of this and add caveats, acknowledging that these are only “European” views and recommendations and that they may not reflect the true needs of the impacted communities.
- Many of the challenges and issues covered in the article are not new. They have not been addressed for many reasons – some are discussed in the manuscript. The article states a target date of 2030 to accomplish some of these while starting some progress on the others. This is a rather tall order. It will be good to discuss what changed over the last few years that make the authors think that there can be significant progress on these challenges, especially noting that CMIP7 timeline is rather short with quite a few of the recommendations need to start very soon, if not now.
- Related to #5 above, I suggest including a review of what the real and perceived impediments have been to date to accomplish the discussed recommendations and a discussion of what the impediments are going forward. Otherwise, I fear that this piece will be another “opinion” piece to be added to the existing ones without really addressing such impediments in a concrete way.
- The manuscript has the feel of written by several authors. I suggest that the lead authors go over the acronyms, definitions, etc. carefully, making the manuscript more coherent. Machine learning is mentioned / discussed as a way forward in many of the sections with similar sentences. Should it have its own section and discussion, perhaps at the end, tying things together? There are also quite a few sentences that are long with multiple groups of a few words separated by commas. Such sentences are rather difficult to parse and understand. An example is the sentence on lines 526-529. Please rephrase these sentences.
Citation: https://doi.org/10.5194/egusphere-2024-453-RC2 -
CC3: 'Comment on egusphere-2024-453 (Dreyfus, Miller & Hull)', Julie Miller, 13 Apr 2024
Comments on Jones et al., 2024
We welcome the opportunity to discuss Jones et al.’s piece “Bringing it all together: Science and modelling priorities to support international climate policy” and submit our comments for consideration by the authors. Our comments are influenced by our perspective as scientists who work at the interface of policy and science. We call attention to the following open questions because greater clarity is needed on these topics to inform current policy discussions. Below, we provide our suggestions for how the modeling community could address these open questions in finer detail and clarity.
Given that we are on the cusp of exceeding 1.5°C, we believe additional thought and investigation are warranted to better characterize the emissions pathways, risks and impacts (reversible and irreversible) that are associated with temporary overshoot. The modeling priorities outlined in your article are an opportunity to provide clarity on (1) what pathways and actions will produce different overshoot scenarios and (2) what the risks and impacts are from those different overshoot scenarios as a function of rate of warming and magnitude and duration of overshoot (see e.g., Reisinger and Geden, 2023).
1. Overshoot & Risk Frameworks
We appreciate how the authors discuss Earth system tipping points specifically in the event of overshoot (Section 3.1 lines 295-305), but propose that the authors explore overshoot impacts more deeply. As a guide, we point the authors to a framework outlined by Reisinger and Geden (2023). In their article, different aspects of overshoot, including peak temperature, overshoot duration, and their integrated sum, are considered for their impact. They ask how these different overshoot aspects are associated with increasing both reversible and irreversible risks. While an overshoot of peak temperature may be temporary, the impacts are not necessarily reversible. We propose that modeling has a role to play in better characterizing these risks and their uncertainties. What modeling approaches and data (observations) are needed to advance this goal? The non-CO2 feedback during overshoot (e.g. methane release from wetlands or permafrost, as noted in line 829) seems to be a major concern but the current ESM capacity in simulating CH4 cycle is low, although some progress is being made with emissions-driven simulations (see e.g., Nzotungicimpaye et al., 2023).
We further propose that both the timeframe of overshoot and the rate of warming are important considerations in this assessment because they may relate to the timeframes over which certain tipping points and HILL events unfold (Ritchie et al., 2023; Lohmann & Ditlevson 2021). The authors already provide important recommendations that HILL events (Section 7.1 lines 604–626) and rapid changes be accounted for in ESMs (Section 9 lines 823-834), and we re-emphasize that these goals be considered within the timeframe of overshoot. To more fully address the role of timeframe, we also suggest the authors investigate both near-term and long-term time windows of overshooting tipping points, such as the next 20, 50, and 100 years, given that this can inform human adaptation. What emission reductions magnitudes and rates plausibly alter the trajectory of these pathways?
2. Overshoot & CDR
Carbon Dioxide Removal (CDR) is a necessary intervention for a temperature exceedance to be temporary, i.e. to be an overshoot. Without CDR or other negative emission or climate intervention, the temperature curve will peak but the accumulated stock of CO2 and ongoing emissions will prevent the curve from bending down. Despite the critical role that CDR plays in our climate goals, its implementation is still largely theoretical. We appreciate the authors surfacing the issue of CDR in their piece (Section 7.3 lines 692-698; Section 9 lines 823-834), and strongly encourage specific focus around its relationship to and constraints on temporary overshoot.
We suggest that the authors consider the recent commentary by Grubert and Talati (2024), where they outline some of the constraints on CDR feasibility, pointing out that the resources and inputs needed for CDR are depletable, and consequently, their implementation will face limits (e.g., finite below-ground storage). They also distinguish between compensatory and actual net-negative CDR, which acknowledges that the amount of CDR available will also be economically limited. We further encourage the authors to consider limitations on BECCS and the time-dependence of emissions and avoiding pathways that result in emissions of irrecoverable carbon (Goldstein et al., 2020).
Given the importance of effective CDR for limiting temporary overshoot, we encourage the authors to explicitly incorporate these knowable limits and constraints into the CDR scenario-making using IAMs (Ramanathan et al., 2021). What do these constraints mean for limitations on the amounts and rates of CDR? How do these feasibility and efficacy limitations place a constraint on the magnitude and timing of overshoot? What are the potential implications for other forms of negative emissions or climate interventions in the context of temporary overshoot and meeting climate goals?
Even assuming future CDR feasibility, there is significant uncertainty over the timing and magnitude of its temperature impact. CO2 removed will have a different temperature impact than if an equivalent amount of CO2 were never emitted (Zickfeld et al., 2023). As a result, preventing CO2 emissions could limit peak warming better than removing an equivalent amount of CO2 through CDR methods. This asymmetry in impact may be due to a variety of factors, including the timing of emissions relative to removals, the effects of co-emitted non-CO2 pollutants, inertia in the climate response, differences in the climate background state, or biogeophysical effects of CDR. Following suggestions made by Zickfeld et al. (2023), we encourage the authors to use ESMs to integrate these different factors and increase certainty about the warming impacts of different CDR scenarios (e.g., reforestation vs. DAC). Distinguishing these non-interchangeable impacts will be essential for clarifying the overshoot peak, timing, and duration of a given pathway.
3. Clearer differentiation between Emulators and ESMs
Given our above recommendations for assessing overshoot warming levels and their impacts, we raise for careful consideration the limitations of climate emulators in these assessments. To what extent can emulators assess the risks associated with overshoot and the feasibility and efficacy of negative GHG emissions? Are there fundamental processes missing from emulators (such as HILL) that would limit their value in such assessment?
4. Clearer differentiation between C1 and C2 overshoot scenarios
IPCC AR6 WGIII established an implicit near-term temperature goal by differentiating between overshoot scenarios: one category of scenarios that stay below 1.5C in 2100 with no or limited overshoot (C1) and the other category of scenarios with high overshoot (C2). We encourage the authors to develop an ensemble of pathways that would elucidate the potential value of an explicit near-term climate goal.
Additionally, more clarity is needed to differentiate among low and high overshoot scenarios. How can improvements in modeling approaches and scenario design better inform this differentiation and its implications for climate policy? Does the realization of different risk levels divide the ensemble into distinct overshoot categories? We further encourage finer differentiation between categories based on their CDR assumptions, particularly for amounts of CDR required by 2050 and 2100. Such recategorization would ideally reflect key CDR differences that are made ambiguous by the current classification based on peak temperature. Finally, consider that more than two categories may be needed to distinguish scenarios along these policy-relevant dimensions.
We thank the authors for raising these questions and appreciate the opportunity to provide comments on how the modeling community can further inform the climate policy discussion on these issues.
Gabrielle B. Dreyfus, Chief Scientist, Institute for Governance & Sustainable Development
Julie S. Miller, Research Associate, Institute for Governance & Sustainable Development
Alyssa Hull, Research Associate, Institute for Governance & Sustainable Development
References
Goldstein A., et al. (2020) Protecting irrecoverable carbon in Earth’s ecosystems, Nat. Clim. Change 10(4): 287–95..
Grubert E. & Talati S. (2024) The distortionary effects of unconstrained for-profit carbon dioxide removal and the need for early governance intervention, Carbon Management 15(1): 1–21.
Lohmann J. & Ditlevsen P. D. (2021) Risk of tipping the overturning circulation due to increasing rates of ice melt, Proceedings of the National Academy of Sciences 118(9): 1-6.
Nzotungicimpaye C.-M., MacIsaac A. J., & Zickfeld K. (2023) Delaying methane mitigation increases the risk of breaching the 2 °C warming limit, Commun Earth Environ 4(1): 1–8.
Ramanathan, V., Xu, Y. & Versaci, A. (2021) Modelling human–natural systems interactions with implications for twenty-first-century warming, Nat Sustain 5: 263-271.
Reisinger A. & Geden O. (2023) Temporary overshoot: Origins, prospects, and a long path ahead, One Earth 6(12): 1631–1637.
Ritchie P. D. L., Alkhayuon H., Cox P. M., & Wieczorek S. (2023) Rate-induced tipping in natural and human systems, Earth System Dynamics 14(3): 669–683.
Zickfeld K., MacIsaac A. J., Canadell J. G., Fuss S., Jackson R. B., Jones C. D., Lohila A., Matthews H. D., Peters G. P., Rogelj J., & Zaehle S. (2023) Net-zero approaches must consider Earth system impacts to achieve climate goals, Nature Climate Change 13(12): 1298–1305.
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CC4: 'Comment on egusphere-2024-453 -- Oliver Morton', Oliver Morton, 13 Apr 2024
Comments on: Bringing it all together: Science and modelling priorities to support international climate policy, Jones et al (Preprint egusphere-2024-453)
The paper identifies “An urgent need to investigate plausible pathways and emission scenarios that realize the Paris Climate Targets including pathways that overshoot the 1.5°C and 2°C targets, before later returning to them” (L81). It treats “What is the feasibility of actually realising the Paris targets?” and “Is it feasible to return to a target warming level on a reasonable timescale once an overshoot has occurred” as “Key questions” (L290). However it says nothing about how “The international modelling community” should address the possibilities of solar geoengineering (also known as Solar Radiation Modification, or SRM) being used in this context.
In AR6 the IPCC notes that “[SR1.5] concluded that SAI could limit warming to below 1.5°C” (4.6.3.3). This strongly suggests that if the modelling community sees the investigation of “plausible pathways…that realize the Paris Climate Targets” it should be looking at this possibility. The IPCC continues “That the climate response to SAI is uncertain and varies across climate models”, highlighting the need for the community’s attention.
To some extent this attention is being provided. A solar-geoengineering scenario (“G6-1.5K-SAI: a new Geoengineering Model Intercomparison Project (GeoMIP) experiment integrating recent advances in solar radiation modification studies”, Daniele Visioni et al, Geoscientific Model Development 17 2583–2596, 2024) was recently included in the CMIP AR7 Fast Track group, which is a good step forward. But the need for more modelling attention to patterns of use and impacts of solar geoengineering is clear. This is true regardless of ex ante positions on the desirability of solar geoengineering approaches under different conditions, which range widely.
Solar geoengineering is under increasing discussion in the policy-adjacent community: see recent publications from UNEP (One Atmosphere: An Independent Expert Review on Solar Radiation Modification Research and Deployment, 2023), the EU (Scoping paper: Solar Radiation Modification by European Commission's Group of Chief Scientific Advisors, 2023), and UNESCO (Report of the World Commission on the Ethics of Scientific Knowledge and Technology (COMEST) on the ethics of climate engineering, 2023) as well as the discussion in the 2023 report of the Climate Overshoot Commission. It is surely incumbent on a modelling community which seeks to “increase the quality and utility of science support to climate policy” by identifying “priority research areas” (L75) to see this discussion unfold in a way informed by the best evidence which climate, earth-system and integrated-assessment models can provide on the potential benefits and drawbacks of solar geoengineering approaches.
In the context of revisions to this paper there would seem to be two ways forward. One would be to expand the relevant sections to include discussion of the need for scenarios which include solar geoengineering and of ways in which modelling within such scenarios could be improved. The alternative would be to include an explanation of the grounds for the authors’ unwillingness to provide such a discussion, lest the paper be mistakenly seen as comprehensive.
Oliver Morton
Senior editor, The Economist
Author, “The Planet Remade”
Chair of the Trustees, The Degrees Initiative
Citation: https://doi.org/10.5194/egusphere-2024-453-CC4
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