Preprints
https://doi.org/10.5194/egusphere-2025-1006
https://doi.org/10.5194/egusphere-2025-1006
26 Mar 2025
 | 26 Mar 2025
Status: this preprint is open for discussion and under review for Geoscientific Model Development (GMD).

The ACCESS-CM2 climate model with a higher resolution ocean-sea ice component (1/4°)

Wilma G. C. Huneke, Andy McC. Hogg, Martin Dix, Daohua Bi, Arnold Sullivan, Shayne McGregor, Chiara Holgate, Siobhan P. O'Farrell, and Micael J. T. Oliveira

Abstract. A new configuration of the Australian Community Climate and Earth System Simulator coupled model, ACCESSCM2, with a higher resolution ocean-sea ice component at 0.25° is introduced. The higher resolution ACCESS-CM2-025 model was developed to better represent the ocean mesoscale and expand the scope of climate modelling research applications. The individual model components have not been changed compared with ACCESS-CM2-1, the existing lower resolution version of the model at 1°, which was one of Australia’s contributions to the World Climate Research Program’s Coupled Model Intercomparison Project Phase 6 (CMIP6). This paper assesses the simulated climate for a 500 year present-day run in ACCESS-CM2-025 against observations, the lower resolution ACCESS-CM2-1 model, and two ocean-sea ice models using the same model components and comparable grid resolutions but with prescribed atmospheric forcing. ACCESS-CM2-025 is more energetic and performs better in regions of elevated ocean mesoscale variability such as at western boundary currents. The higher resolution ACCESS-CM2-025 also features a more realistic ENSO life cycle and seasonality, with a reduced biennality, which is common in the lower resolution ACCESS-CM2-1. Both ACCESS-CM2 models share many biases, particularly near the sea surface and also affecting sea ice coverage, reflecting insufficiency in the atmospheric model component. While ACCESS-CM2-025 exhibits improved time-mean deep convection, sea ice, and mixed layer depth in the North Atlantic, it also experiences multidecadal variability, which is evident in many variables, including the Atlantic Meridional Overturning Circulation.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
Share
Wilma G. C. Huneke, Andy McC. Hogg, Martin Dix, Daohua Bi, Arnold Sullivan, Shayne McGregor, Chiara Holgate, Siobhan P. O'Farrell, and Micael J. T. Oliveira

Status: open (until 21 May 2025)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
Wilma G. C. Huneke, Andy McC. Hogg, Martin Dix, Daohua Bi, Arnold Sullivan, Shayne McGregor, Chiara Holgate, Siobhan P. O'Farrell, and Micael J. T. Oliveira
Wilma G. C. Huneke, Andy McC. Hogg, Martin Dix, Daohua Bi, Arnold Sullivan, Shayne McGregor, Chiara Holgate, Siobhan P. O'Farrell, and Micael J. T. Oliveira

Viewed

Total article views: 130 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
98 29 3 130 4 4
  • HTML: 98
  • PDF: 29
  • XML: 3
  • Total: 130
  • BibTeX: 4
  • EndNote: 4
Views and downloads (calculated since 26 Mar 2025)
Cumulative views and downloads (calculated since 26 Mar 2025)

Viewed (geographical distribution)

Total article views: 128 (including HTML, PDF, and XML) Thereof 128 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 23 Apr 2025
Download
Short summary
A new configuration of the Australian Community Climate and Earth System Simulator coupled model, ACCESS-CM2, with a higher resolution ocean-sea ice component is introduced. The new version of the coupled climate model was designed to better capture smaller-scale ocean motions. While this configuration improves the representation of many aspects of the climate system, some biases from the existing lower-resolution version persist.
Share