Computational framework for the Earth system modelling and the INM-CM6 climate model implemented on its base
Abstract In this paper, we present the current stage of development of the INM-CM Earth system model family by the Marchuk Institute of Numerical Mathematics of the Russian Academy of Sciences. The major change from the previous model version INM-CM5 is a new computational platform for the Earth System modelling. We describe the main parts of this digital platform, such as ocean-atmosphere coupling, version control, compilation/configuration, and automated testing subsystems. We also discuss major modifications of the physical parts of the climate model whereby the model simulations of observed climate were significantly improved as well as the model computational performance.
Authors
- M. A. Tarasevich
- Andrey Gritsun (ORCID: https://orcid.org/0000-0002-1595-1787)
- Sergey S. Petrov (ORCID: https://orcid.org/0000-0001-5702-1126)
- E. M. Volodin (ORCID: https://orcid.org/0000-0003-1073-7287)
- Ilya Chernov (ORCID: https://orcid.org/0000-0001-7479-9079)
- S. V. Kostrykin
- Nikolay Iakovlev (ORCID: https://orcid.org/0000-0003-2573-728X)
- Rostislav Yu. Fadeev (ORCID: https://orcid.org/0000-0002-3928-9986)
- Dmitry V. Blagodatskikh (ORCID: https://orcid.org/0009-0008-1402-9038)
- A. Yu. Chernenkov (ORCID: https://orcid.org/0000-0003-0195-7608)
- I. V. Tsybulin
- Vladimir A. Onoprienko (ORCID: https://orcid.org/0009-0003-1320-4774)
- Alisa A. Ezhkova
- V. V. Bragina
Institutions
- Hydrometeorological Research Centre of Russian Federation (RU)
- Moscow Institute of Physics and Technology (RU)
- Institute of Numerical Mathematics (RU)
- Institute of Geography (RU)
- Institute of Global Climate and Ecology (RU)
- Yandex (Russia) (RU)
Publication Details
- Journal
- Russian Journal of Numerical Analysis and Mathematical Modelling
- Published
- 2024-11-28
- DOI
- https://doi.org/10.1515/rnam-2024-0032
- Citations
- 11
- Primary Topic
- Climate variability and models
- Type
- article
- Field-Weighted Citation Impact
- 3.11