Abstract
We present direct numerical simulations of the different two-dimensional flow regimes generated by a constant spatially periodic forcing balanced by viscous dissipation and large scale drag with a dimensionless damping rate . The linear response to the forcing is a square array of counter-rotating vortices, which is stable when the Reynolds number or are small. After identifying the sequence of bifurcations that lead to a spatially and temporally chaotic regime of the flow when and are increased, we study the transitions between the different turbulent regimes observed for large by varying . A large scale circulation at the box size (the condensate state) is the dominant mode in the limit of vanishing large scale drag ( large). When is decreased, the condensate becomes unstable and a regime with random reversals between two large scale circulations of opposite signs is generated. It involves a bimodal probability density function of the large scale velocity that continuously bifurcates to a Gaussian distribution when is decreased further.
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