Before revision: Glacial regime Glacial regime of the Kander (Switzerland) The glacial regime is characterised by: Very high discharge in summer after the ice melt Very low discharge from the end of autumn to early spring Amplitude of monthly variation of discharge greater than 25 Very high daily variability in discharge during the year High flow (several hundred l/s/km2) It is found at high altitudes, above .
After revision: Simple regime is where all rivers have one peak discharge per yearGlacial regime Glacial regime of the Kander (Switzerland) The glacial regime is characterised by: Very high discharge in summer after the ice melt Very low discharge from the end of autumn to early spring Amplitude of monthly variation of discharge greater than 25 Very high daily variability in discharge during the year High flow (several hundred l/s/km2) It is found at high altitudes, above .