“…As was previously found [16], three distinctive regimes for the driving at finite rates can be identified: slow, intermediate and fast rate regime. When the change of the external field is very slow, similarly as in the adiabatic case [13,15,17,18], avalanches propagate individually, well separated in time, which allows statistical interpretation of distributions of their parameters (such as size and duration). However, in most of experimental realizations the driving rate is finite [19,20].…”