Articles | Volume 19, issue 5
https://doi.org/10.5194/gmd-19-1809-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
A Climate Intervention Dynamical Emulator (CIDER) for scenario space exploration
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- Final revised paper (published on 04 Mar 2026)
- Preprint (discussion started on 21 May 2025)
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
| : Report abuse
- RC1: 'Comment on egusphere-2025-1830', Anonymous Referee #1, 01 Jun 2025
- RC2: 'Comment on egusphere-2025-1830', Anonymous Referee #2, 08 Jul 2025
- AC1: 'Comment on egusphere-2025-1830', Jared Farley, 10 Oct 2025
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Jared Farley on behalf of the Authors (07 Nov 2025)
Author's response
Author's tracked changes
Manuscript
ED: Referee Nomination & Report Request started (14 Nov 2025) by Yongze Song
RR by Anonymous Referee #2 (18 Nov 2025)
RR by Anonymous Referee #3 (06 Jan 2026)
ED: Publish as is (27 Jan 2026) by Yongze Song
AR by Jared Farley on behalf of the Authors (06 Feb 2026)
Manuscript
I recommend this paper be accepted, subject to addressing the following concerns:
Yes, the paper shows that the emulator can produce output for some variable that are linearly related to forcing. But I think the entire project needs to be framed more clearly. Some of these points are addressed in the discussion, but they need to be added to the abstract. What can the emulator not do? What is its purpose? Because it does not include a seasonal cycle in the resulting maps of temperature and precipitation, it cannot be used for many potential impacts of climate change that matter, such as food production and water resources. It cannot simulate monsoon impacts. It cannot simulate the diurnal cycle, which is important for many impacts, including agriculture and tropospheric ozone. It does not include downward diffuse vs. direct radiation, or UV. And because the two GCMs used as examples differ quite a bit in some aspects, any actual use of the emulator would require multiple climate models so as to add a probability distribution to the resulting emulated climate.
Will it be possible to also emulate impacts of SRM in addition to the standard climate variables of temperature, precipitation, and evaporation? What would it take? And can the authors add warnings about the usage of emulators prominently in their abstract and introduction?
The way the emulator works is to include CO2-equivalent and SO2 time series of forcing, but no mention is made of tropospheric aerosols, land use, and other forcings included in SSPs. How are they handled?
Please also address the 40 comments in the attached annotated manuscript.
Technical issues:
Cider is not brewed. It is fermented. So the title to section 2 needs to be changed. See the comments in the attached annotated manuscript.
Your model nomenclature is confusing. You have CESM2(WACCM), CESM2-WACCM6, and CESM2. Are these all the same? Then use the same notation. The same for UKESM1 and UKESM1.0.
There are several acronyms that are not defined.
You use “validation” multiple times, when you mean “evaluation.” “Validation” means that you are proving that the model works, that it is valid.
Multiple references in the text do not use parentheses around the years.