Fig. 4: Gaussian process (GP) emulation for sea level contribution at t = 150 years. | Communications Earth & Environment

Fig. 4: Gaussian process (GP) emulation for sea level contribution at t = 150 years.

From: Calculations of extreme sea level rise scenarios are strongly dependent on ice sheet model resolution

Fig. 4

a–g SLC computed as a function of the average melt rate at t = 0, denoted \({M}_{{t}_{0}}\): a GP model was fitted separately for each resolution from R = 2 km to R = 8 km. The black crosses show the WAVI output, the blue line is the predicted mean and the shaded area shows the confidence of the GP model (97.5th percentile of the data).

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