The Community Earth System Model Version 2 (CESM2)
Danabasoglu, G., Lamarque, J., Bacmeister, J., Bailey, D. A., DuVivier, A. K. , et al. (2020). The Community Earth System Model Version 2 (CESM2). Journal of Advances in Modeling Earth Systems, doi:10.1029/2019MS001916
| Title | The Community Earth System Model Version 2 (CESM2) |
|---|---|
| Author(s) | Gokhan Danabasoglu, Jean-Francois Lamarque, Julio Bacmeister, David A. Bailey, Alice K. DuVivier, James Edwards, Louisa K. Emmons, John Fasullo, Rolando Garcia, Andrew Gettelman, Cecile Hannay, Marika M. Holland, William G. Large, Peter H. Lauritzen, David M. Lawrence, Jan T. M. Lenaerts, Keith Lindsay, William H. Lipscomb, Michael J. Mills, Richard Neale, Keith W. Oleson, Bette Otto‐Bliesner, Adam S. Phillips, William Sacks, Simone Tilmes, L. Kampenhout, Mariana Vertenstein, Alice Bertini, John Dennis, Clara Deser, Chris Fischer, B. Fox‐Kemper, J. E. Kay, Douglas Kinnison, P. J. Kushner, V. E. Larson, Matthew C. Long, Sheri Mickelson, J. K. Moore, Eris Nienhouse, L. Polvani, P. J. Rasch, Warren G. Strand |
| Abstract | An overview of the Community Earth System Model Version 2 (CESM2) is provided, including a discussion of the challenges encountered during its development and how they were addressed. In addition, an evaluation of a pair of CESM2 long preindustrial control and historical ensemble simulations is presented. These simulations were performed using the nominal 1 degrees horizontal resolution configuration of the coupled model with both the "low-top" (40 km, with limited chemistry) and "high-top" (130 km, with comprehensive chemistry) versions of the atmospheric component. CESM2 contains many substantial science and infrastructure improvements and new capabilities since its previous major release, CESM1, resulting in improved historical simulations in comparison to CESM1 and available observations. These include major reductions in low-latitude precipitation and shortwave cloud forcing biases; better representation of the Madden-Julian Oscillation; better El Nino-Southern Oscillation-related teleconnections; and a global land carbon accumulation trend that agrees well with observationally based estimates. Most tropospheric and surface features of the low- and high-top simulations are very similar to each other, so these improvements are present in both configurations. CESM2 has an equilibrium climate sensitivity of 5.1-5.3 degrees C, larger than in CESM1, primarily due to a combination of relatively small changes to cloud microphysics and boundary layer parameters. In contrast, CESM2's transient climate response of 1.9-2.0 degrees C is comparable to that of CESM1. The model outputs from these and many other simulations are available to the research community, and they represent CESM2's contributions to the Coupled Model Intercomparison Project Phase 6. |
| Publication Title | Journal of Advances in Modeling Earth Systems |
| Publication Date | Feb 6, 2020 |
| Publisher's Version of Record | https://dx.doi.org/10.1029/2019MS001916 |
| OpenSky Citable URL | https://n2t.net/ark:/85065/d7v98c85 |
| OpenSky Listing | View on OpenSky |
| CISL Affiliations | TDD, ASAP, IOWA, ISD, SAGE |