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Accretion of protoplanetary discs (PPDs) could be driven by MHD disc winds rather than turbulent viscosity. With a dynamical prescription for angular momentum transport induced by disc winds, we perform 2D simulations of PPDs to systematically investigate the rate and direction of planet migration in a windy disc. We find that the the strength of disc winds influences the corotation region similarly to the "desaturation" effect of viscosity. The magnitude and direction of torque depend sensitively on the hierarchy between the radial advection timescale across the horseshoe due to disc wind $\tau_{\rm dw}$, the horsehoe libration timescale $\tau_{\rm lib}$ and U-turn timescale $\tau_{\rm U-turn}$. Initially, as wind strength increases and the advection timescale shortens, a non-linear horseshoe drag emerges when $\tau_{\rm dw} \lesssim \tau_{\rm lib}$, which tends to drive strong outward migration. Subsequently, the drag becomes linear and planets typically still migrate inward when $\tau_{\rm dw} \lesssim \tau_{\rm U-turn} \sim \tau_{\rm lib}h$, where $h$ is the disc aspect ratio. The range of outward migration between two transitions corresponds to $\sim $ 10-100 au in a realistic PPD for a planet with mass ratio of $\sim 10^{-5}$.