... | ... | @@ -9,7 +9,7 @@ I used 3 different domains for the SST restoring experiments: |
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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)
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3) Barents Sea Opening (BSO), between 70N and 77N and between 16E and 20E.
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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.
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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.
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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).
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