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Update SST restoring experiments authored by David Docquier's avatar David Docquier
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SST-restoring-experiments.md
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......@@ -40,7 +40,7 @@ increase is much lower compared to BSO and Fram; and the changes in OHT at Davis
- Fig. 10: the mean March sea-ice thickness decreases everywhere in the Arctic in all experiments, especially in the North Atlantic experiments (top row); as for sea-ice concentration, increasing the SST in the North Atlantic experiment (top row, from left to right) clearly decreases the sea-ice thickness, but this sea-ice thinning clearly spans the whole Arctic.
![OHT_50yrs_SST](uploads/0e0f5ac54f9496657c6f3dec54f5a5a5/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)**
**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) are plotted for reference; the number in brackets is the difference in mean OHT between the experiment and the control (CTRL)**
![OHT_Total_timeseries_SST](uploads/5b5ac21e139a8765b4124f8de4f8b3fc/OHT_Total_timeseries_SST.png)
**Fig. 2: Time series of annual mean OHT through all Arctic straits (BSO + Fram Strait + Bering Strait + Davis Strait); the number in brackets is the difference in mean OHT between the experiment and the control (CTRL)**
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