The DOE E3SM Coupled Model Version 1: Overview and evaluation at standard resolution
This work documents the first version of the U.S. Department of Energy (DOE) new Energy Exascale Earth System Model (E3SMv1). We focus on the standard resolution of the fully coupled physical model designed to address DOE mission‐relevant water cycle questions. Its components include atmosphere and...
Published in: | Journal of Advances in Modeling Earth Systems |
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Other Authors: | , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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2019
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Online Access: | https://doi.org/10.1029/2018MS001603 |
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description |
This work documents the first version of the U.S. Department of Energy (DOE) new Energy Exascale Earth System Model (E3SMv1). We focus on the standard resolution of the fully coupled physical model designed to address DOE mission‐relevant water cycle questions. Its components include atmosphere and land (110‐km grid spacing), ocean and sea ice (60 km in the midlatitudes and 30 km at the equator and poles), and river transport (55 km) models. This base configuration will also serve as a foundation for additional configurations exploring higher horizontal resolution as well as augmented capabilities in the form of biogeochemistry and cryosphere configurations. The performance of E3SMv1 is evaluated by means of a standard set of Coupled Model Intercomparison Project Phase 6 (CMIP6) Diagnosis, Evaluation, and Characterization of Klima simulations consisting of a long preindustrial control, historical simulations (ensembles of fully coupled and prescribed SSTs) as well as idealized CO2 forcing simulations. The model performs well overall with biases typical of other CMIP‐class models, although the simulated Atlantic Meridional Overturning Circulation is weaker than many CMIP‐class models. While the E3SMv1 historical ensemble captures the bulk of the observed warming between preindustrial (1850) and present day, the trajectory of the warming diverges from observations in the second half of the twentieth century with a period of delayed warming followed by an excessive warming trend. Using a two‐layer energy balance model, we attribute this divergence to the model's strong aerosol‐related effective radiative forcing (ERFari+aci = −1.65 W/m2) and high equilibrium climate sensitivity (ECS = 5.3 K). 1852977 |
author2 |
Golaz, Jean‐Christophe (author) Caldwell, Peter M. (author) Van Roekel, Luke P. (author) Petersen, Mark R. (author) Tang, Qi (author) Wolfe, Jonathan D. (author) Abeshu, Guta (author) Anantharaj, Valentine (author) Asay‐Davis, Xylar S. (author) Bader, David C. (author) Baldwin, Sterling A. (author) Bisht, Gautam (author) Bogenschutz, Peter A. (author) Branstetter, Marcia (author) Brunke, Michael A. (author) Brus, Steven R. (author) Burrows, Susannah M. (author) Cameron‐Smith, Philip J. (author) Donahue, Aaron S. (author) Deakin, Michael (author) Easter, Richard C. (author) Evans, Katherine J. (author) Feng, Yan (author) Flanner, Mark (author) Foucar, James G. (author) Fyke, Jeremy G. (author) Griffin, Brian M. (author) Hannay, Cécile (author) Harrop, Bryce E. (author) Hoffman, Mattthew J. (author) Hunke, Elizabeth C. (author) Jacob, Robert L. (author) Jacobsen, Douglas W. (author) Jeffery, Nicole (author) Jones, Philip W. (author) Keen, Noel D. (author) Klein, Stephen A. (author) Larson, Vincent E. (author) Leung, L. Ruby (author) Li, Hong‐Yi (author) Lin, Wuyin (author) Lipscomb, William H. (author) Ma, Po‐Lun (author) Mahajan, Salil (author) Maltrud, Mathew E. (author) Mametjanov, Azamat (author) McClean, Julie L. (author) McCoy, Renata B. (author) Neale, Richard B. (author) Price, Stephen F. (author) |
format |
Article in Journal/Newspaper |
title |
The DOE E3SM Coupled Model Version 1: Overview and evaluation at standard resolution |
spellingShingle |
The DOE E3SM Coupled Model Version 1: Overview and evaluation at standard resolution |
title_short |
The DOE E3SM Coupled Model Version 1: Overview and evaluation at standard resolution |
title_full |
The DOE E3SM Coupled Model Version 1: Overview and evaluation at standard resolution |
title_fullStr |
The DOE E3SM Coupled Model Version 1: Overview and evaluation at standard resolution |
title_full_unstemmed |
The DOE E3SM Coupled Model Version 1: Overview and evaluation at standard resolution |
title_sort |
doe e3sm coupled model version 1: overview and evaluation at standard resolution |
publishDate |
2019 |
url |
https://doi.org/10.1029/2018MS001603 |
genre |
Sea ice |
genre_facet |
Sea ice |
op_relation |
Journal of Advances in Modeling Earth Systems--J. Adv. Model. Earth Syst.--1942-2466--1942-2466 input4MIPs.SOLARIS-HEPPA.solar.CMIP.SOLARIS-HEPPA-3-2--10.22033/ESGF/input4MIPs.1122 Sea Ice Concentrations from Nimbus-7 SMMR and DMSP SSM/I-SSMIS Passive Microwave Data, Version 1--10.5067/8GQ8LZQVL0VL NOAA/NSIDC Climate Data Record of Passive Microwave Sea Ice Concentration, Version 3--10.7265/N59P2ZTG Extended Reconstructed Sea Surface Temperature (ERSST), Version 4--10.7289/V5KD1VVF Atlantic meridional overturning circulation observed by the RAPID-MOCHA-WBTS (RAPID-Meridional Overturning Circulation and Heatflux Array-Western Boundary Time Series) array at 26N from 2004 to 2017.--10.5285/5acfd143-1104-7b58-e053-6c86abc0d94b Cice-Consortium/Icepack Version 1.0.2--10.5281/zenodo.1213463 E3Sm-Project/A-Prime: A-Prime Release Version V1.2--10.5281/zenodo.1311053 Historical Emissions (1750 - 2014) - CEDS - v2017-05-18--10.22033/ESGF/input4MIPs.1241 Biomass Burning emissions for CMIP6 (v1.2)--10.22033/ESGF/input4MIPs.1117 NOAA Global Surface Temperature Dataset, Version 4.0--10.7289/v5fn144h articles:22756 ark:/85065/d72v2d94 doi:10.1029/2018MS001603 |
op_rights |
Copyright 2019 American Geophysical Union. |
op_doi |
https://doi.org/10.1029/2018MS001603 |
container_title |
Journal of Advances in Modeling Earth Systems |
container_volume |
11 |
container_issue |
7 |
container_start_page |
2089 |
op_container_end_page |
2129 |
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1766195294654955520 |
spelling |
ftncar:oai:drupal-site.org:articles_22756 2023-05-15T18:18:39+02:00 The DOE E3SM Coupled Model Version 1: Overview and evaluation at standard resolution Golaz, Jean‐Christophe (author) Caldwell, Peter M. (author) Van Roekel, Luke P. (author) Petersen, Mark R. (author) Tang, Qi (author) Wolfe, Jonathan D. (author) Abeshu, Guta (author) Anantharaj, Valentine (author) Asay‐Davis, Xylar S. (author) Bader, David C. (author) Baldwin, Sterling A. (author) Bisht, Gautam (author) Bogenschutz, Peter A. (author) Branstetter, Marcia (author) Brunke, Michael A. (author) Brus, Steven R. (author) Burrows, Susannah M. (author) Cameron‐Smith, Philip J. (author) Donahue, Aaron S. (author) Deakin, Michael (author) Easter, Richard C. (author) Evans, Katherine J. (author) Feng, Yan (author) Flanner, Mark (author) Foucar, James G. (author) Fyke, Jeremy G. (author) Griffin, Brian M. (author) Hannay, Cécile (author) Harrop, Bryce E. (author) Hoffman, Mattthew J. (author) Hunke, Elizabeth C. (author) Jacob, Robert L. (author) Jacobsen, Douglas W. (author) Jeffery, Nicole (author) Jones, Philip W. (author) Keen, Noel D. (author) Klein, Stephen A. (author) Larson, Vincent E. (author) Leung, L. Ruby (author) Li, Hong‐Yi (author) Lin, Wuyin (author) Lipscomb, William H. (author) Ma, Po‐Lun (author) Mahajan, Salil (author) Maltrud, Mathew E. (author) Mametjanov, Azamat (author) McClean, Julie L. (author) McCoy, Renata B. (author) Neale, Richard B. (author) Price, Stephen F. (author) 2019-08-08 https://doi.org/10.1029/2018MS001603 en eng Journal of Advances in Modeling Earth Systems--J. Adv. Model. Earth Syst.--1942-2466--1942-2466 input4MIPs.SOLARIS-HEPPA.solar.CMIP.SOLARIS-HEPPA-3-2--10.22033/ESGF/input4MIPs.1122 Sea Ice Concentrations from Nimbus-7 SMMR and DMSP SSM/I-SSMIS Passive Microwave Data, Version 1--10.5067/8GQ8LZQVL0VL NOAA/NSIDC Climate Data Record of Passive Microwave Sea Ice Concentration, Version 3--10.7265/N59P2ZTG Extended Reconstructed Sea Surface Temperature (ERSST), Version 4--10.7289/V5KD1VVF Atlantic meridional overturning circulation observed by the RAPID-MOCHA-WBTS (RAPID-Meridional Overturning Circulation and Heatflux Array-Western Boundary Time Series) array at 26N from 2004 to 2017.--10.5285/5acfd143-1104-7b58-e053-6c86abc0d94b Cice-Consortium/Icepack Version 1.0.2--10.5281/zenodo.1213463 E3Sm-Project/A-Prime: A-Prime Release Version V1.2--10.5281/zenodo.1311053 Historical Emissions (1750 - 2014) - CEDS - v2017-05-18--10.22033/ESGF/input4MIPs.1241 Biomass Burning emissions for CMIP6 (v1.2)--10.22033/ESGF/input4MIPs.1117 NOAA Global Surface Temperature Dataset, Version 4.0--10.7289/v5fn144h articles:22756 ark:/85065/d72v2d94 doi:10.1029/2018MS001603 Copyright 2019 American Geophysical Union. article Text 2019 ftncar https://doi.org/10.1029/2018MS001603 2022-08-09T18:22:52Z This work documents the first version of the U.S. Department of Energy (DOE) new Energy Exascale Earth System Model (E3SMv1). We focus on the standard resolution of the fully coupled physical model designed to address DOE mission‐relevant water cycle questions. Its components include atmosphere and land (110‐km grid spacing), ocean and sea ice (60 km in the midlatitudes and 30 km at the equator and poles), and river transport (55 km) models. This base configuration will also serve as a foundation for additional configurations exploring higher horizontal resolution as well as augmented capabilities in the form of biogeochemistry and cryosphere configurations. The performance of E3SMv1 is evaluated by means of a standard set of Coupled Model Intercomparison Project Phase 6 (CMIP6) Diagnosis, Evaluation, and Characterization of Klima simulations consisting of a long preindustrial control, historical simulations (ensembles of fully coupled and prescribed SSTs) as well as idealized CO2 forcing simulations. The model performs well overall with biases typical of other CMIP‐class models, although the simulated Atlantic Meridional Overturning Circulation is weaker than many CMIP‐class models. While the E3SMv1 historical ensemble captures the bulk of the observed warming between preindustrial (1850) and present day, the trajectory of the warming diverges from observations in the second half of the twentieth century with a period of delayed warming followed by an excessive warming trend. Using a two‐layer energy balance model, we attribute this divergence to the model's strong aerosol‐related effective radiative forcing (ERFari+aci = −1.65 W/m2) and high equilibrium climate sensitivity (ECS = 5.3 K). 1852977 Article in Journal/Newspaper Sea ice OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Journal of Advances in Modeling Earth Systems 11 7 2089 2129 |