Articles | Volume 19, issue 8
https://doi.org/10.5194/gmd-19-3395-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Assessing resolution sensitivity in coupled climate simulations with AWI-CM3
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- Final revised paper (published on 27 Apr 2026)
- Preprint (discussion started on 20 Jan 2026)
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-2025-5061', Anonymous Referee #1, 11 Mar 2026
- AC2: 'Reply on RC1', Martina Zapponini, 27 Mar 2026
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RC2: 'Comment on egusphere-2025-5061', Anonymous Referee #2, 16 Mar 2026
- AC1: 'Reply on RC2', Martina Zapponini, 18 Mar 2026
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Martina Zapponini on behalf of the Authors (30 Mar 2026)
Author's response
Author's tracked changes
Manuscript
ED: Publish as is (13 Apr 2026) by Paul Ullrich
AR by Martina Zapponini on behalf of the Authors (16 Apr 2026)
Manuscript
General comments:
The paper provides a useful overview of the coupled AWI-CM3 model, providing a near direct comparison between two model resolutions, as well as evaluation against observations/re-analysis and CMIP6. Particular attention is given to polar climate, where increased resolution has a larger impact on mesoscale processes unresolved by coarser resolution. The comparison is between a pair of simulations from 1950 - 2100, with most of the emphasis on evaluation of biases relative to present-day observations or reanalysis, rather than on future projections. Overall this is a well-written and clearly understandable manuscript that provides a very useful benchmark for the AWI-CM3 model and the impact of increased resolution.
Specific comments:
Each model is run for 250 years from initialization in repeat 1950 conditions, with the first 100 years considered spinup and subsequent 150 years as control. It would be useful to have some mention of the model’s level of equilibrium during this control period, and/or see metrics. Figure 3 shows some of this; the global SST and 2m air temperatures seem to be in equilibrium in the control, but maybe some of the sea ice metrics have a trend during the control? Is the ocean steadily gaining or losing heat during the control? In Figure 7d the AMOC time series appear to be declining from 1950, was this trend also in the control?