Preprints
https://doi.org/10.5194/egusphere-2026-1676
https://doi.org/10.5194/egusphere-2026-1676
14 Apr 2026
 | 14 Apr 2026
Status: this preprint is open for discussion and under review for Geoscientific Model Development (GMD).

UKCM2-LL: a new low-resolution GC5 configuration with constrained climate sensitivity – methodology and development

John W. Rostron, Alejandro Bodas-Salcedo, David M. H. Sexton, Colin G. Jones, Edward W. Blockley, Till Kuhlbrodt, Jane P. Mulcahy, Tamzin E. Palmer, Saloua Peatier, Mark A. Ringer, Steven T. Rumbold, Benjamin M. Sanderson, Yongming Tang, and Martin R. Willet

Abstract. The Global Coupled model version 5 (GC5) of the Met Office Unified Model incorporates substantial developments across its model components and shows improved performance for a range of applications. However, it exhibits a very high effective climate sensitivity (EffCS) of 6.7 K and an excessive rise in recent global-mean surface air temperatures (GMSAT), limiting its suitability for some climate applications. This motivated the development of an alternative GC5-based configuration with EffCS constrained to lie within the IPCC Sixth Assessment Report “very likely” range, improved simulation of historical temperatures, and acceptable climatological performance. This new configuration, called UKCM2-LL, will form part of the UK’s submission to CMIP7.

We describe a two-stage methodology used to develop UKCM2-LL. First, a 503-member atmosphere-only perturbed parameter ensemble (PPE) of GC5 variants was used to train statistical emulators that predict climatological performance metrics and atmosphere-only feedbacks. These emulators were then used to generate 41 candidate configurations predicted to have substantially reduced EffCS relative to GC5. Second, coupled preindustrial control and abrupt 4×CO₂ experiments were used to evaluate the candidates against large-scale climatological metrics and to diagnose EffCS, progressively narrowing the set of viable configurations through an expert-led evaluation process. Final fine-tuning of a single candidate was performed manually using the coupled experiments and was informed by parameter sensitivity information derived from the PPE. The resulting UKCM2-LL configuration has an EffCS of 3.6 K and exhibits an improved simulation of historical temperatures relative to GC5. However, achieving this lower EffCS required a degradation in climatological performance, reflecting a structural constraint of the GC5 model.

This work demonstrates the value of PPE-based approaches for systematically exploring such structural constraints, and for parameter tuning during model development. We discuss potential improvements to the methodology and consider the implications of explicitly constraining climate sensitivity for future model development and multi-model ensemble diversity.

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John W. Rostron, Alejandro Bodas-Salcedo, David M. H. Sexton, Colin G. Jones, Edward W. Blockley, Till Kuhlbrodt, Jane P. Mulcahy, Tamzin E. Palmer, Saloua Peatier, Mark A. Ringer, Steven T. Rumbold, Benjamin M. Sanderson, Yongming Tang, and Martin R. Willet

Status: open (until 09 Jun 2026)

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John W. Rostron, Alejandro Bodas-Salcedo, David M. H. Sexton, Colin G. Jones, Edward W. Blockley, Till Kuhlbrodt, Jane P. Mulcahy, Tamzin E. Palmer, Saloua Peatier, Mark A. Ringer, Steven T. Rumbold, Benjamin M. Sanderson, Yongming Tang, and Martin R. Willet

Data sets

Supplementary material for manuscript "UKCM2-LL: a new low-resolution GC5 configuration with constrained climate sensitivity – methodology and development": Data John W. Rostron and David M. H. Sexton https://doi.org/10.5281/zenodo.19267353

Model code and software

Supplementary material for manuscript "UKCM2-LL: a new low-resolution GC5 configuration with constrained climate sensitivity – methodology and development": Scripts John W. Rostron https://doi.org/10.5281/zenodo.19205160

John W. Rostron, Alejandro Bodas-Salcedo, David M. H. Sexton, Colin G. Jones, Edward W. Blockley, Till Kuhlbrodt, Jane P. Mulcahy, Tamzin E. Palmer, Saloua Peatier, Mark A. Ringer, Steven T. Rumbold, Benjamin M. Sanderson, Yongming Tang, and Martin R. Willet
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Latest update: 14 Apr 2026
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Short summary
The Met Office’s latest weather and climate model warms very strongly in response to increases in carbon dioxide. We created a modified version of the model with a more moderate warming response by adjusting key model parameters, using both automated methods and expert judgement. The new model matches historical temperatures more closely and is better suited for studies of long‑term climate, but has reduced overall accuracy when simulating the baseline climate.
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