Fig. 3
Dependence of amplitudes (left) and periods (right) of the vertical oscillation on the rain mass fraction μ at the beginning (ξ01, P1) and end (ξ02, P2) of the simulation. Values for low mass condensation regions for which the plasma remains trapped at the loop apex are shown in red. The solid line shows amplitudes predicted by 1D mechanical model by Verwichte et al. (2017).
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