Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled ocean-atmopshere-sea ice configuration. This dataset contains all data necessary to reproduce figures and analysis published in Roquet et al. (2022). It includes outputs from the ocean, atmosphere, sea ice, and land surface components of the MITgcm simulations of the Control simulation and sensitivity experiments. Outputs cover the last 50 years of all simulations after spin-up. Roquet, F., D. Ferreira, R. Caneill, D. Schlesinger, and G. Madec, 2022: Unique thermal expansion properties of water key to the formation of sea ice on Earth. Science Advances. DOI:10.1126/sciadv.abq079
International audienceThe formation of sea ice in polar regions is possible because a salinity gradi...
Sea ice is a key element of the Earth's climate system, and also of significant ecological, geo‐poli...
International audienceThe formation of sea ice in polar regions is possible because a salinity gradi...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
International audienceThe formation of sea ice in polar regions is possible because a salinity gradi...
Sea ice is a key element of the Earth's climate system, and also of significant ecological, geo‐poli...
International audienceThe formation of sea ice in polar regions is possible because a salinity gradi...
International audienceThe formation of sea ice in polar regions is possible because a salinity gradi...
Sea ice is a key element of the Earth's climate system, and also of significant ecological, geo‐poli...
International audienceThe formation of sea ice in polar regions is possible because a salinity gradi...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
International audienceThe formation of sea ice in polar regions is possible because a salinity gradi...
Sea ice is a key element of the Earth's climate system, and also of significant ecological, geo‐poli...
International audienceThe formation of sea ice in polar regions is possible because a salinity gradi...
International audienceThe formation of sea ice in polar regions is possible because a salinity gradi...
Sea ice is a key element of the Earth's climate system, and also of significant ecological, geo‐poli...
International audienceThe formation of sea ice in polar regions is possible because a salinity gradi...