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April 15, 2026Journal of Advances in Modeling Earth Systems2 citationsOpen Access

The Energy Exascale Earth System Model Version 3: 2. Overview of the Coupled System

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JGJean‐Christophe GolazWLWuyin LinBrookhaven National LaboratoryXZXue ZhengYunnan Agricultural University

Key Points

  • This research aims to present the advancements in the Energy Exascale Earth System Model version 3 (E3SMv3).
  • Development of coupled components to enhance model fidelity
  • Incorporation of advanced atmospheric chemistry and microphysics
  • Implementation of new ocean mesh with sub‐ice‐shelf cavities
  • Testing through comprehensive simulation campaigns from 1850 to 2024
  • Integration of prognostic vegetation dynamics and improved solar radiation treatment
  • Enhanced modeling of historical surface temperature reduces earlier bias
  • Improved alignment with observational data through reduced aerosol-related forcing
  • Refined ocean heat content and sea ice trends as a result of updates
  • Better simulation of cryospheric processes through advanced snow and ice physics

Abstract

Abstract The Energy Exascale Earth System Model version 3 (E3SMv3) represents the latest advancement in Earth system modeling developed by the U.S. Department of Energy (DOE). Building upon previous versions, E3SMv3 introduces significant updates across its coupled components to enhance capability and improve fidelity. The atmosphere component incorporates advancements in chemistry, aerosol‐cloud interactions, convection, and microphysics. The ocean features a new time‐stepping scheme and a higher‐resolution unstructured mesh with sub‐ice‐shelf cavities, while the sea ice model integrates advanced snow and ice physics for more realistic cryospheric simulations. The land model introduces prognostic vegetation dynamics and a new sub‐grid topographic treatment of solar radiation. A new tri‐grid configuration harmonizes the horizontal grids of the land and river components for improved process coupling. It is enabled by a new non‐linear remapping between the atmosphere and land. E3SMv3 underwent extensive testing through a comprehensive simulation campaign, including pre‐industrial control, idealized experiments, and historical simulations spanning 1850–2024. The model demonstrates significant improvements in simulating the evolution of the historical surface temperature, particularly addressing the “pothole cooling” bias in earlier versions. Reduced aerosol‐related forcing contributes to more realistic radiative forcing and better alignment with the observational record. Ocean heat content (OHC) and sea ice trends are also improved as a result.

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Cite This Study

Golaz et al. (2026) studied this question.

synapsesocial.com/papers/69df2ba0e4eeef8a2a6b0a0bhttps://doi.org/10.1029/2025ms005302
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