Articles | Volume 11, issue 2
https://doi.org/10.5194/gmd-11-713-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gmd-11-713-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The sea ice model component of HadGEM3-GC3.1
Jeff K. Ridley
CORRESPONDING AUTHOR
Met Office, Exeter, EX1 3PB, UK
Edward W. Blockley
Met Office, Exeter, EX1 3PB, UK
Ann B. Keen
Met Office, Exeter, EX1 3PB, UK
Jamie G. L. Rae
Met Office, Exeter, EX1 3PB, UK
Alex E. West
Met Office, Exeter, EX1 3PB, UK
David Schroeder
Department of Meteorology, University of Reading, Reading, RG6 6BB, UK
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- Mechanisms of Internal Atlantic Multidecadal Variability in HadGEM3-GC3.1 at Two Different Resolutions W. Lai et al. 10.1175/JCLI-D-21-0281.1
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- The Met Office Global Coupled Model 3.0 and 3.1 (GC3.0 and GC3.1) Configurations K. Williams et al. 10.1002/2017MS001115
- U.K. Community Earth System Modeling for CMIP6 C. Senior et al. 10.1029/2019MS002004
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Latest update: 05 Dec 2024
Short summary
The sea ice component of the Met Office coupled climate model, HadGEM3-GC3.1, is presented and evaluated. We determine that the mean state of the sea ice is well reproduced for the Arctic; however, a warm sea surface temperature bias over the Southern Ocean results in a low Antarctic sea ice cover.
The sea ice component of the Met Office coupled climate model, HadGEM3-GC3.1, is presented and...