We investigate a model of thin layer turbulence that follows the evolution of the two-dimensional motions u2D(x,y) along the horizontal directions $(x,y)$ coupled to a single Fourier mode along the vertical direction ( z ) of the form uq(x,y,z)=[vₓ(x,y)sin (qz),vy(x,y)sin (qz),vz(x,y)cos (qz)] , reducing thus the system to two coupled, two-dimensional equations. The model, despite its simplicity and ad hoc construction, displays a rich behaviour. Its reduced dimensionality allows a thorough investigation of the transition from a forward to an inverse cascade of energy as the thickness of the layer H=[STIX]x03C0/q is varied. Starting from a thick layer and reducing its thickness it is shown that two critical heights are met: (i) one for which the forward unidirectional cascade (similar to three-dimensional turbulence) transitions to a bidirectional cascade transferring energy to both small and large scales and (ii) one for which the bidirectional cascade transitions to a unidirectional inverse cascade when the layer becomes very thin (similar to two-dimensional turbulence). The two critical heights are shown to have different properties close to criticality that we are able to analyse with numerical simulations for a wide range of Reynolds numbers and aspect ratios.
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