SST-restoring-experiments.md

@@ -26,7 +26,7 @@ Here are the different model experiments with the corresponding color in the plo
 increase is much lower compared to BSO and Fram; amd the changes in OHT at Davis Strait are very small in all experiments (not shown);
 - Figs. 5 and 6: the total Arctic-sea ice area (SIA) and volume (SIV) decrease in all experiments with SST increase, in agreement with the OHT increase; the strength of the SIA decrease is higher with increased SST for the 2 first domains, but not for the BSO domain (where the strength of the SIA decrease is relatively similar between the 3 experiments);
 - Fig. 7: the spatial extent of the SST increase follows the domain used for the SST restoring, with a larger spatial extent in the SST increase with the larger domain;
-- Fig. 8: the mixed layer depth in the Labrador and Greenland-Iceland-Norway (GIN) Seas decreases with SST increase for the 2 larger domains (North Atlantic and northern North Atlantic); this probably explains the OHT decreases south of 60N, following a weakening of the overturning circulation.
+- Fig. 8: the mixed layer depth in the Labrador, northern North Atlantic and Greenland-Iceland-Norway (GIN) Seas decreases with SST increase for the 2 larger domains (North Atlantic and northern North Atlantic); this probably explains the OHT decreases south of 60N, following a weakening of the overturning circulation.
 
 ![OHT_50yrs_SST](uploads/db9cbd926edb0406000f254b8b61d963/OHT_50yrs_SST.png)
 **Fig. 1: Latitudinal transect of mean Atlantic OHT averaged over 50 years (except 2000-2014 for the CMIP6 r1 member to compare to TF2017); OHT estimates from Trenberth and Fasullo (TF2017) and hydrographic measurements (as in Grist et al., 2018) are plotted for reference; the number in brackets is the difference in mean OHT between the experiment and the control (CTRL)**