“…Several findings have suggested that wall-bounded turbulent flows can take different statistically stationary turbulent states, with different length scale of the flow structures and with different transport properties, even for the very same values of the control parameters. Examples for the coexistence of such multiple turbulent states include turbulent (rotating) Rayleigh-Bénard convection [2][3][4][5][6][7][8], Taylor-Couette turbulence [9][10][11], double-diffusive convection turbulence [12], von Karman flow [13][14][15][16], rotating spherical Couette flow [17], Couette flow with span-wise rotation [18], but also geophysical flows [19,20] such as in ocean circulation [21][22][23], in the liquid metal core of Earth [24][25][26][27], or in the atmosphere [28,29].…”