@@ -9,9 +9,9 @@ I used 3 different domains for the SST restoring experiments:
2) Northern North Atlantic, between 66N and 80N and between 22W and 20E
3) Barents Sea Opening (BSO), between 70N and 77N and between 16E and 20E.
I have applied a SST restoring to the mean climatology of the period 2100-2129 (30 years) plus 1°C, 3°C and 5°C, respectively, for the 3 different domains described above, resulting in 9 different sensitivity experiments, which can be compared to the control run.
I have applied a SST restoring to the mean climatology of the period 2100-2129 (30 years) plus 1°C, 3°C and 5°C, respectively, for the 3 different domains described above, resulting in 9 different sensitivity experiments, which can be compared to the control run. In order not to have too sharp gradients in SST (and other resulting variables), I have applied a 9-point smoothing at the borders of the domains.
More information about the methodology can be found in [Ruprich-Robert et al. (2017)](https://journals.ametsoc.org/doi/full/10.1175/JCLI-D-16-0127.1).
Based on the SST restoring information, the model computes the corresponding surface heat flux correction in the domain of interest. More information about the methodology can be found in [Ruprich-Robert et al. (2017)](https://journals.ametsoc.org/doi/full/10.1175/JCLI-D-16-0127.1).
Here are the different model experiments with the corresponding color in the plots below:
-**t613 (red solid curve, run by K. Wyser)** is the CMIP6 EC-Earth3-Veg r1 historical member covering 1850-2014 (only the period 1950-2014 is shown here);
