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Update CMIP6 authored by David Docquier's avatar David Docquier
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......@@ -38,9 +38,9 @@ Fig. 4: Latitudinal transect of northward Indo-Pacific ocean heat transport (OHT
Fig. 5: Time series of northward Atlantic ocean heat transport (OHT) at (a) 60N and (b) 70N. The thick black solid line is the OHT estimate from Trenberth et al. (2019). The number in brackets indicates the number of members to compute the mean OHT for each model.
![SIA_March-OHT_atl_70N](uploads/f3dd1e9c08d061cc092eff3a54c9b919/SIA_March-OHT_atl_70N.png)
Fig. 6: Scatter plots of detrended March Arctic sea-ice area against detrended annual mean Atlantic ocean heat transport at 70N for all points between 1950 and 2014. We show results only from the 5 best CMIP6 models in terms of historical Arctic SIA, SIV and Atlantic OHT, as well as observations/reanalysis in the bottom right panel (OSI SAF for sea-ice area and Trenberth et al. (2019) estimate for ocean heat transport). The correlation coefficients *R* and regression slopes *a* (unit: 1000 km^2 per TW) are shown in the upper right corner of each panel for each model.
Fig. 6: Scatter plots of detrended March Arctic sea-ice area against detrended annual mean Atlantic ocean heat transport at 70N for all points between 1950 and 2014. We show results only from the 5 best CMIP6 models in terms of historical Arctic SIA and Atlantic OHT, as well as observations/reanalysis in the bottom right panel (OSI SAF for sea-ice area and Trenberth et al. (2019) estimate for ocean heat transport). The correlation coefficients *R* and regression slopes *a* (unit: 1000 km^2 per TW) are shown in the upper right corner of each panel for each model.
![SIV_March-OHT_atl_70N](uploads/4acda2abce91dff9b687976a97e18168/SIV_March-OHT_atl_70N.png)
Fig. 7: Scatter plots of detrended March Arctic sea-ice volume against detrended annual mean Atlantic ocean heat transport for all points between 1950 and 2014. We show results only from the 5 best CMIP6 models in terms of historical Arctic SIA, SIV and Atlantic OHT, as well as reanalysis in the bottom right panel (PIOMAS for sea-ice volume and Trenberth et al. (2019) estimate for ocean heat transport). The correlation coefficients *R* and regression slopes *a* (unit: km^3 per TW) are shown in the upper right corner of each panel for each model.
Fig. 7: Scatter plots of detrended March Arctic sea-ice volume against detrended annual mean Atlantic ocean heat transport for all points between 1950 and 2014. We show results only from the 5 best CMIP6 models in terms of historical Arctic SIA and Atlantic OHT, as well as reanalysis in the bottom right panel (PIOMAS for sea-ice volume and Trenberth et al. (2019) estimate for ocean heat transport). The correlation coefficients *R* and regression slopes *a* (unit: km^3 per TW) are shown in the upper right corner of each panel for each model.
Important note: These figures were produced by D. Docquier and constitute preliminary results (not published in papers).
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