Data used to create Experiment 1 figure

Four model simulations from Experiment One in "Potential Ice Sheet Modulation of Volcanism in West Antarctica: Constraints on the cadence and magnitude of melt delivery into the crust" using the numerical model developed in the paper. Mantle heat injection is held effectively constant and an insulating boundary layer (ice sheet) is introduced once a steady state is reached.Time is measured relative to one characteristic diffusion timescale tau_d ~ 6 Myr.