Cyclic reformation of subcritical perpendicular fast magnetosonic shocks due to oblique Whistler waves
Two-dimensional PIC simulations reveal that subcritical perpendicular fast magnetosonic shocks undergo cyclic reformation driven by an oblique lower-hybrid gradient drift instability, where the coupling between backward-propagating oblique Whistler waves and forward-propagating ion acoustic waves modulates the magnetic field and forces the shock to collapse and reform without external perturbations.