SST-restoring-experiments.md

@@ -9,7 +9,7 @@ I used 3 different domains for the SST restoring experiments:
 2) Northern North Atlantic, between 66N (latitude of Iceland) and 80N (latitude of Svalbard)) and between 22W (longitude of East Greenland) and 20E (longitude of BSO)
 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. 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.
+I have applied a SST restoring to the mean climatology of the period 2100-2129 (30 years) in my control run 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.
 
 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).