Fig. 2: Projected 2m temperature changes for the end of the twenty-first century (2070–2099, relative to 1990–2019) in the JJA (June–July–August) and DJF (December–January–February) seasons. | Nature Communications

Fig. 2: Projected 2m temperature changes for the end of the twenty-first century (2070–2099, relative to 1990–2019) in the JJA (June–July–August) and DJF (December–January–February) seasons.

From: Delayed Antarctic sea-ice decline in high-resolution climate change simulations

Fig. 2

The projections with the a, d high-resolution (HR) and b, e low-resolution (LR) model configurations are based on a Representative high-emission Concentration Pathway (RCP8.5 scenario). Differences in the climate response for c, f the HR and LR projections (HR-LR) are most pronounced in the Southern Hemisphere. A “delta approach”, as outlined by the HighResMIP protocol (High-Resolution Model Intercomparison Project, see “Methods”), has been applied to isolate the climate change signal. The ocean grid spacing for g HR and h LR is given as a multiple of the local i, Rossby radius R of deformation (“Methods”).

Back to article page