The DOE E3SM Model Version 2: Overview of the Physical Model and Initial Model Evaluation

Jean Christophe Golaz, Luke P. Van Roekel, Xue Zheng, Andrew F. Roberts, Jonathan D. Wolfe, Wuyin Lin, Andrew M. Bradley, Qi Tang, Mathew E. Maltrud, Ryan M. Forsyth, Chengzhu Zhang, Tian Zhou, Kai Zhang, Charles S. Zender, Mingxuan Wu, Hailong Wang, Adrian K. Turner, Balwinder Singh, Jadwiga H. Richter, Yi QinMark R. Petersen, Azamat Mametjanov, Po Lun Ma, Vincent E. Larson, Jayesh Krishna, Noel D. Keen, Nicole Jeffery, Elizabeth C. Hunke, Walter M. Hannah, Oksana Guba, Brian M. Griffin, Yan Feng, Darren Engwirda, Alan V. Di Vittorio, Cheng Dang, Le Ann M. Conlon, Chih Chieh Jack Chen, Michael A. Brunke, Gautam Bisht, James J. Benedict, Xylar S. Asay-Davis, Yuying Zhang, Meng Zhang, Xubin Zeng, Shaocheng Xie, Phillip J. Wolfram, Tom Vo, Milena Veneziani, Teklu K. Tesfa, Sarat Sreepathi, Andrew G. Salinger, J. E.Jack Reeves Eyre, Michael J. Prather, Salil Mahajan, Qing Li, Philip W. Jones, Robert L. Jacob, Gunther W. Huebler, Xianglei Huang, Benjamin R. Hillman, Bryce E. Harrop, James G. Foucar, Yilin Fang, Darin S. Comeau, Peter M. Caldwell, Tony Bartoletti, Karthik Balaguru, Mark A. Taylor, Renata B. McCoy, L. Ruby Leung, David C. Bader

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Abstract

This work documents version two of the Department of Energy's Energy Exascale Earth System Model (E3SM). E3SMv2 is a significant evolution from its predecessor E3SMv1, resulting in a model that is nearly twice as fast and with a simulated climate that is improved in many metrics. We describe the physical climate model in its lower horizontal resolution configuration consisting of 110 km atmosphere, 165 km land, 0.5° river routing model, and an ocean and sea ice with mesh spacing varying between 60 km in the mid-latitudes and 30 km at the equator and poles. The model performance is evaluated with Coupled Model Intercomparison Project Phase 6 Diagnosis, Evaluation, and Characterization of Klima simulations augmented with historical simulations as well as simulations to evaluate impacts of different forcing agents. The simulated climate has many realistic features of the climate system, with notable improvements in clouds and precipitation compared to E3SMv1. E3SMv1 suffered from an excessively high equilibrium climate sensitivity (ECS) of 5.3 K. In E3SMv2, ECS is reduced to 4.0 K which is now within the plausible range based on a recent World Climate Research Program assessment. However, a number of important biases remain including a weak Atlantic Meridional Overturning Circulation, deficiencies in the characteristics and spectral distribution of tropical atmospheric variability, and a significant underestimation of the observed warming in the second half of the historical period. An analysis of single-forcing simulations indicates that correcting the historical temperature bias would require a substantial reduction in the magnitude of the aerosol-related forcing.

Original languageEnglish
Article numbere2022MS003156
JournalJournal of Advances in Modeling Earth Systems
Volume14
Issue number12
DOIs
StatePublished - Dec 2022

Funding

The authors are grateful to three anonymous reviewers for their constructive suggestions, which significantly improved the manuscript. This research was supported as part of the E3SM project, funded by the U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research. E3SM production simulations were performed on a high-performance computing cluster provided by the BER ESM program and operated by the Laboratory Computing Resource Center at Argonne National Laboratory. Developmental simulations were also performed using BER ESM program's Compy computing cluster located at Pacific Northwest National Laboratory. Additional developmental simulations, as well as post-processing and data archiving of production simulations used resources of the National Energy Research Scientific Computing Center (NERSC), a DOE Office of Science User Facility supported by the Office of Science of the U.S. Department of Energy under Contract No. DE-AC02-05CH11231. This work was partially supported by the National Center for Atmospheric Research, which is a major facility sponsored by the National Science Foundation under Cooperative Agreement 1852977. Portions of this study were supported by the Regional and Global Model Analysis (RGMA) component of the Earth and Environmental System Modeling Program of the U.S. Department of Energy's Office of Biological and Environmental Research (BER) via NSF Interagency Agreement 1844590. Lawrence Livermore National Laboratory is operated by Lawrence Livermore National Security, LLC, for the U.S. Department of Energy, National Nuclear Security Administration under Contract DE-AC52-07NA27344. Sandia National Laboratories is a multimission laboratory managed and operated by National Technology and Engineering Solutions of Sandia, LLC., a wholly owned subsidiary of Honeywell International, Inc., for the U.S. Department of Energy's National Nuclear Security Administration under contract DE-NA-0003525. Pacific Northwest National Laboratory is operated by Battelle for the U.S. Department of Energy under Contract DE-AC05-76RL01830. This paper describes objective technical results and analysis. Any subjective views or opinions that might be expressed in the paper do not necessarily represent the views of the U.S. Department of Energy or the United States Government. The authors are grateful to three anonymous reviewers for their constructive suggestions, which significantly improved the manuscript. This research was supported as part of the E3SM project, funded by the U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research. E3SM production simulations were performed on a high‐performance computing cluster provided by the BER ESM program and operated by the Laboratory Computing Resource Center at Argonne National Laboratory. Developmental simulations were also performed using BER ESM program's Compy computing cluster located at Pacific Northwest National Laboratory. Additional developmental simulations, as well as post‐processing and data archiving of production simulations used resources of the National Energy Research Scientific Computing Center (NERSC), a DOE Office of Science User Facility supported by the Office of Science of the U.S. Department of Energy under Contract No. DE‐AC02‐05CH11231. This work was partially supported by the National Center for Atmospheric Research, which is a major facility sponsored by the National Science Foundation under Cooperative Agreement 1852977. Portions of this study were supported by the Regional and Global Model Analysis (RGMA) component of the Earth and Environmental System Modeling Program of the U.S. Department of Energy's Office of Biological and Environmental Research (BER) via NSF Interagency Agreement 1844590. Lawrence Livermore National Laboratory is operated by Lawrence Livermore National Security, LLC, for the U.S. Department of Energy, National Nuclear Security Administration under Contract DE‐AC52‐07NA27344. Sandia National Laboratories is a multimission laboratory managed and operated by National Technology and Engineering Solutions of Sandia, LLC., a wholly owned subsidiary of Honeywell International, Inc., for the U.S. Department of Energy's National Nuclear Security Administration under contract DE‐NA‐0003525. Pacific Northwest National Laboratory is operated by Battelle for the U.S. Department of Energy under Contract DE‐AC05‐76RL01830. This paper describes objective technical results and analysis. Any subjective views or opinions that might be expressed in the paper do not necessarily represent the views of the U.S. Department of Energy or the United States Government.

FundersFunder number
National Science Foundation1844590, 1852977
U.S. Department of Energy
National Center for Atmospheric Research
Office of ScienceDE‐AC02‐05CH11231
National Nuclear Security AdministrationDE‐AC52‐07NA27344, DE‐NA‐0003525, DE‐AC05‐76RL01830
Biological and Environmental Research
Argonne National Laboratory
Pacific Northwest National Laboratory
Laboratory Computing Resource Center

    Keywords

    • DOE E3SM
    • climate modeling

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