For a solenoidal three-component velocity depending on two periodic coordinates and a zero-mean magnetic field with the same dependence, the in-plane flux potential satisfies a homogeneous advection-diffusion equation. The Poincaré inequality gives . Integrating the vertical stretching term by parts bounds it by , where . Maximizing against resistive dissipation and integrating gives the displayed transient bound. Splitting off half the dissipation instead gives , proving vertical energy decays. This permits transient generation by a nonzero vertical velocity while excluding sustained fields in this zero-mean, z-independent periodic class.

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