Atlantic-and-Pacific-SST-experiments.md

@@ -19,12 +19,14 @@ Here are the different model experiments with the corresponding color in the plo
 - Fig. 6: the OHT at the BSO increases in all experiments, but much more clearly in the North Atlantic experiment;
 - Fig. 7: the OHT at the Bering Strait increases in all experiments, but more markedly in the North Pacific and Bering Strait experiments;
 - Fig. 8: the OHT at the Fram Strait generally increases in the wide and middle domain experiments, but with much lower amplitude compared to the increased OHT at the BSO and Bering Strait.
+- Fig. 9: the AMOC index at 26.5N decreases in the wide and middle domain experiments, which partly explains the decreased OHT south of 60N;
+
 
 ![OHT_50yrs_APSST](uploads/da02abde0371b6180cb9c4382901c44b/OHT_50yrs_APSST.png)
 **Fig. 1: Latitudinal transect of mean Atlantic OHT averaged over 50 years for the control run and the 3 Atlantic (top panel) and 3 Pacific (bottom) experiments; the number in brackets is the difference in mean OHT between the experiment and the control (CTRL)**
 
 ![Maps_March_SST_diff_APSST](uploads/8698ca88467f17de0d5b50044cd7a591/Maps_March_SST_diff_APSST.png)
-**Fig. 2: Maps of difference in mean SST, averaged over 50 years, between the Atlantic (top row) / Pacific (bottom) experiments and the control run**
+**Fig. 2: Maps of difference in mean March SST, averaged over 50 years, between the Atlantic (top row) / Pacific (bottom) experiments and the control run**
 
 ![SIA_Cycle_APSST](uploads/d5074ff3a3a773ad7c088b81e09009d0/SIA_Cycle_APSST.png)
 **Fig. 3: Mean seasonal cycle of Arctic sea-ice area (SIA), averaged over 50 years, for the control run and the 3 Atlantic (left panel) and 3 Pacific (right panel) experiments; the numbers in brackets are the differences in mean SIA in March/September between the experiment and the control (CTRL)**
@@ -42,4 +44,10 @@ Here are the different model experiments with the corresponding color in the plo
 **Fig. 7: Time series of ocean heat transport (OHT) at the Bering Strait for the control run and the 3 Atlantic (top panel) and 3 Pacific (bottom panel) experiments; the number in brackets is the difference in mean OHT between the experiment and the control (CTRL)**
 
 ![OHT_Fram_timeseries_APSST](uploads/686929d6f8de4aa459cbaa670882f500/OHT_Fram_timeseries_APSST.png)
-**Fig. 8: Time series of ocean heat transport (OHT) at the Fram Strait for the control run and the 3 Atlantic (top panel) and 3 Pacific (bottom panel) experiments; the number in brackets is the difference in mean OHT between the experiment and the control (CTRL)**
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+**Fig. 8: Time series of ocean heat transport (OHT) at the Fram Strait for the control run and the 3 Atlantic (top panel) and 3 Pacific (bottom panel) experiments; the number in brackets is the difference in mean OHT between the experiment and the control (CTRL)**
+
+![AMOC_APSST](uploads/ce5887194439a27f0cae52bba83e13ba/AMOC_APSST.png)
+**Fig. 9: Time series of Atlantic Meridional Overturning Circulation (AMOC) index at 26.5N (maximum Atlantic meridional stream function between 900 and 1200m) for the control run and the 3 Atlantic (top panel) and 3 Pacific (bottom panel) experiments**
+
+![zomsfatl_50yrs_diff_APSST](uploads/164e1b97ba5e9fe5674a45650b406d21/zomsfatl_50yrs_diff_APSST.png)
+**Fig. 10: Vertical profiles of the difference in Atlantic meridional stream function (AMSF) between the Atlantic (top panel) / Pacific (bottom panel) experiments and the control run, averaged over 50 years**
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