Extended Data Fig. 6: Objective construction of the model ensemble solution. | Nature Geoscience

Extended Data Fig. 6: Objective construction of the model ensemble solution.

From: Abrupt changes in the global carbon cycle during the last glacial period

Extended Data Fig. 6

Left panel. The forcings that enter the model with variable scaling (AABW formation scaled to WD-δ18O Antarctic sea-ice extent scaled to the log of WD Na, Subantarctic PO4 scaled to WD-Ca, and NADW formation scaled to Bermuda Rise Pa/Th, not shown Antarctic PO4 scaled to a combination of WD-Ca and sea ice extent). The maximum possible forcing is shown with the dotted red line along with the associated model response of atmospheric CO2 (black line). The red shading shows the range of forcings (mean and 1-sigma) that produce model predictions consistent with the ice core data (that is the ‘combined scenario’). The middle panel shows the same 1-sigma range for temperature forcings in the ‘combined scenario’. The right panel shows various model predictions including those that are used to select the ‘combined scenario’ constraint: atmospheric CO2, atmospheric δ13C-CO2 (including spline-smoothed data from refs. 44,59,60) and mean ocean temperature (MOT). All model results are slightly offset to match interglacial values in the data. Blue bars show the temporal range used in for each data constraint.

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