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|  |  | The goal of the [OSeaIce projet](https://cordis.europa.eu/project/id/834493) is to explore the two-way interactions between ocean heat transport and Arctic sea ice, using the [EC-Earth](http://www.ec-earth.org/) coupled atmosphere-ocean global climate model. A depiction of the main ocean currents going to the Arctic is shown in the figure below. | 
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|  |  | Figure: Ocean circulation in the Arctic with the main currents. The Atlantic Water (in red) is one of the main drivers of Arctic sea-ice changes [Credit: Fig. 3 of [Carmack et al. (2015)](https://doi.org/10.1175/BAMS-D-13-00177.1)]. | 
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|  |  | So far, I have performed two types of model sensitivity experiments with EC-Earth3.3.1.1 (NEMO3.6-LIM3 ocean-sea ice model coupled to IFS cycle 36r4 atmosphere model) using T255-ORCA1 grids (100km nominal resolution in both the atmosphere and ocean): | 
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|  |  | 1) [Global experiments](Global experiments): experiments in which I modified the value of certain ocean coefficients globally (e.g. eddy viscosity, bottom drag coefficient) | 
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|  |  | 2) [SST restoring experiments](SST restoring experiments): experiments in which I restored the SST in a selected region to a certain value. | 
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|  |  | Please let me know if you have any question or comment regarding this project: david.docquier@smhi.se | 
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|  |  | Please let me know if you have any question or comment regarding this project: [david.docquier@smhi.se](david.docquier@smhi.se) | 
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|  |  | **Figure: Ocean circulation in the Arctic with the main currents. The Atlantic Water (in red) is one of the main drivers of Arctic sea-ice changes [Credit: Fig. 3 of [Carmack et al. (2015)](https://doi.org/10.1175/BAMS-D-13-00177.1)].** | 
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