In a steady axisymmetric magnetohydrodynamic wind, axisymmetric pressure and Newtonian gravity exert no azimuthal torque. The azimuthal momentum equation is . Mass conservation and the solenoidal vector field condition imply . With magnetohydrodynamic mass loading , the transported angular momentum per unit poloidal magnetic flux is . It is constant on connected regular poloidal flux surfaces. The usual specific magnetohydrodynamic angular-momentum invariant is , provided ; confusing these two normalizations loses a factor of mass loading in the wind torque.

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