“…When Ha ∼ O(1), equation (2.4) may be used as the upstream flow in a slowly varying channel, a situation that allows a direct interaction between the applied magnetic field and the viscous flow throughout the channel. In particular, when Re 1, (x, y, t) = (Re X, y, Re T) and (u, v, p) ∼ (U, Re −1 V, P) + · · · , then the flow is known to be governed by the following boundary layer problem (see Genin & Podshibyakin [5], which is also documented in Blūms et al [3] for zero magnetic field (Ha = 0).…”