Design and implementation of the infrastructure of HadGEM3: the next-generation Met Office climate modelling system
By Helene Hewitt, D. Copsey, I. Culverwell, C. Harris, R. Hill, A. Keen, A. McLaren, Elizabeth C. Hunke. 2010
390 citations recorded by the source corpus.
Abstract. This paper describes the development of a technically robust climate modelling system, HadGEM3, which couples the Met Office Unified Model atmosphere component, the NEMO ocean model and the Los Alamos sea ice model (CICE) using the OASIS coupler. Details of the coupling and technical solutions of the physical model (HadGEM3-AO) are documented, in addition to a description of the configurations of the individual submodels. The paper demonstrates that the implementation of the model has resulted in accurate conservation of heat and freshwater across the model components. The model performance in early versions of this climate model is briefly described to demonstrate that the results are scientifically credible. HadGEM3-AO is the basis for a number of modelling efforts outside of the Met Office, both within the UK and internationally. This documentation of the HadGEM3-AO system provides a detailed reference for developers of HadGEM3-based climate configurations.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/c9eed2dd63798abec683142086f7ce6791328440
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In Atmospheric Science
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Citations in the corpus
- Improved Atlantic winter blocking in a climate model (2011, methodology): “[5] We use the Hadley Centre Global Environmental Model version 3 (HadGEM3) [Hewitt et al., 2010; Arribas et al., 2011].”
- A mechanism for lagged North Atlantic climate response to solar variability (2013, methodology): “[5] To investigate the coupled ocean-atmosphere response to solar variability, we first use experiments with the third Hadley Centre Global Environmental Model (HadGEM3) [Hewitt et al., 2010].”
- The Canadian Earth System Model version 5 (CanESM5.0.3) (2019, methodology): “4.1, likely arise from the use of the linear free surface (Madec and the NEMO team, 2012), and have been seen in previous coupled models using NEMO (Hewitt et al., 2011).”
- The CNRM-CM5.1 global climate model: description and basic evaluation (2013, neutral): “The model had only 31 vertical levels on a z-grid, but with a resolution in the upper 100 meters similar to ORCA-1 .”