Abstract. -The field induced switching of conductance in the charge ordered half-doped manganites is controlled by the combination of metastability, an inhomogeneous high field state, and cation disorder. We study this non-equilibrium problem via real space Monte Carlo on a disordered strong coupling model appropriate to the manganites. We reproduce the variation of the switching fields with the mean ionic radius rA and cation disorder σA, and demonstrate how the experimental features arise from the proximity of several phases in the Landau free energy landscape. Our prediction for the field melted state is consistent with a growing body of experimental evidence.The manganites owe their fame to the 'colossal magnetoresistance' effect, whereby an applied magnetic field strongly suppresses the resistance of the material. The most extreme version of this happens when the field can actually induce an insulator-metal transition (IMT). This occurs in the low bandwidth half doped manganites, e.g, Pr 0.5 Ca 0.5 MnO 3 , that are typically charge ordered (CO) insulators with CE magnetic order [1][2][3]. The CE-CO-I state is transformed to a ferromagnetic metal (FM-M) by an applied field through a first order phase transition. The magnetic field induced conversion of the CE order to FM, and the crucial resistive switching, involve several subtleties which are only gradually being appreciated [4][5][6][7][8][9][10][11][12][13][14]. These include the surprising difference between the melting fields in two lanthanide (Ln) families, namely the Ca [4] and the Sr [5,6] families; the smallness of the field melting energy scales [4][5][6][7]; and the spatial character of field induced melting and its relation to structural disorder [8][9][10][11][12]. We expand on these issues below.(i) The phase boundary between the CE and FM phase is first order, so metastable states exist on either side. This leads to hysteresis, and the switching fields are decided by non-equilibrium effects, not free energy balance.(ii) While trapping into metastable states is expected in a first order transition, an applied field leads to new equilibrium states which are not simple continuation of the zero field state. In particular, it is increasingly apparent that the field induced conducting state is an inhomogeneous FM-M, a percolative metal with a finite volume fraction of charge ordered regions [8][9][10][11][12]. Finally, (iii) the field induced switching and inhomogeneous metallicity play out on a structurally disordered background. One expects the CO-I state to be more stable in narrow band systems. While this is true in the Ca based manganites [4], where the cation size mismatch σ A is small, it is completely opposite in the Sr based systems [5,6]. The more insulating system can be driven metallic easier in the presence of disorder! These three actors, metastability, field induced inhomogeneity, and pinning disorder, enrich and complicate the field melting problem. There is no understanding of their interplay in the field induced IMT, and the noneq...