Assessing Earth's Energy Imbalance Trend in the Early 21st Century in Two High‐Resolution Coupled Models

Abstract Satellite observations since 2001 show an increasing Earth's energy imbalance (EEI) at the top of the atmosphere of 0.45 W m −2 dec −1 , a trend understated in coupled climate models. We assess the 2001–2024 EEI trend in historical simulations of two high‐resolution coupled models, CM4X, a revised version of CM4.0, and CESM‐HR, a high‐resolution version of CESM1, each with 10 realizations. The ensemble‐mean EEI trends in CM4X and CESM‐HR capture only 25% and 55% of the observed trend, respectively, due to underestimated shortwave trends in the tropics and Southern Hemisphere extratropics. CESM‐HR exhibits twice the intramodel variability in EEI and surface warming trends than CM4X, and biases in EEI trends are not linked to warming‐pattern differences. One CESM‐HR realization matches the observed EEI trend but via strong Antarctic offshore polynyas absent from observations. These results highlight the potentially critical influence of sea‐ice processes on near‐term climate projections in high‐resolution models.

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Publication Details

Journal
Geophysical Research Letters
Published
2026-04-30
DOI
https://doi.org/10.1029/2025gl121277
Primary Topic
Climate variability and models
Type
article
Field-Weighted Citation Impact
0.00

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article

Assessing Earth's Energy Imbalance Trend in the Early 21st Century in Two High‐Resolution Coupled Models

Timothy M. Merlis, Yu Chen, Stephan A. Fueglistaler, Tra Dinh et al.
Geophysical Research Letters
Climate variability and models
article

Assessing Earth's Energy Imbalance Trend in the Early 21st Century in Two High‐Resolution Coupled Models

Timothy M. Merlis, Yu Chen, Stephan A. Fueglistaler, Tra Dinh, Raphaël Dussin, Stephen M. Griffies, Niki Zadeh, John Krasting
article en

Abstract

Abstract Satellite observations since 2001 show an increasing Earth's energy imbalance (EEI) at the top of the atmosphere of 0.45 W m −2 dec −1 , a trend understated in coupled climate models. We assess the 2001–2024 EEI trend in historical simulations of two high‐resolution coupled models, CM4X, a revised version of CM4.0, and CESM‐HR, a high‐resolution version of CESM1, each with 10 realizations. The ensemble‐mean EEI trends in CM4X and CESM‐HR capture only 25% and 55% of the observed trend, respectively, due to underestimated shortwave trends in the tropics and Southern Hemisphere extratropics. CESM‐HR exhibits twice the intramodel variability in EEI and surface warming trends than CM4X, and biases in EEI trends are not linked to warming‐pattern differences. One CESM‐HR realization matches the observed EEI trend but via strong Antarctic offshore polynyas absent from observations. These results highlight the potentially critical influence of sea‐ice processes on near‐term climate projections in high‐resolution models.

Geophysical Research LettersVol. 53(9)
Centre National de la Recherche Scientifique (FR), NOAA Geophysical Fluid Dynamics Laboratory (US), Princeton University (US), University Corporation for Atmospheric Research (US), Sorbonne Université (FR), Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (FR), Institut de Recherche pour le Développement (FR)
U.S. Department of Commerce
Climate action
Openalex Percentile: Top 6%
Climate variability and models
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