Results of Experiment Two

Five model simulations from Experiment Two 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. Average Mantle heat injection rate is held constant while the period of oscillation for heat injection is different for each simulation.Time is measured relative to one characteristic diffusion timescale tau_d ~ 6 Myr.