For the isothermal equation of state, , with constant isothermal sound speed . A nonzero steady plane-parallel flow has constant mass flux . Choose the positive flow direction for convenience. The continuity equation then gives , and the steady Euler momentum equation becomesIntegrating and absorbing the reference velocity into the constant yields, for the Mach number ,For the opposite flow direction use ; the same relation holds.
A smooth sonic point has , so its momentum equation requires . Moreover satisfies , and has its minimum . Thus, if the flow reaches at ,A sonic crossing is therefore possible at a maximum of the potential, withAt a nondegenerate maximum, the expansions give . Choosing either smooth sign gives a crossing slope , joining a subsonic flow to a supersonic flow, or the reverse. This establishes the plane-parallel isothermal sonic transition at a potential maximum. For a globally defined crossing, the same maximum must also be high enough for the Bernoulli relation to remain real over the intended domain.
Decompose and . In a steady axisymmetric vector field, and . The radial and vertical components of its curl areTherefore is a constant. Regularity at the symmetry axis sets ; equivalently, one imposes no toroidal loop electromotive force, . Under this usual condition,which implieswhere . This is the regular-axis alignment of steady poloidal ideal flow. It allows nonzero toroidal components as well.
The axis or zero-loop-voltage condition is necessary for the unqualified conclusion. On an annular domain, and give with zero curl, yet the poloidal vectors are perpendicular. This can satisfy the remaining steady equations as well: choose constant mass density , and on the annulus. The field has zero curl, radial pressure balances gravity, the flow advects no equilibrium quantity, and . It carries a nonzero loop voltage. Steady axisymmetry alone on an annulus therefore does not exclude such cross-field flow.
Use the aligned poloidal flow from part (i), and define the magnetohydrodynamic mass loading , so . Axisymmetric mass conservation and give . Introduce the poloidal magnetic flux function by , and write . ThenThe steady induction equation says the curl of this expression is zero. Hence , wherethe field-line angular velocity is constant on each connected magnetic surface and along its field lines.
To control the difference between matter rotation and field-line rotation, use the azimuthal component of the ideal magnetohydrodynamic momentum equation. The inertial and magnetic terms are respectively and ; pressure and gravity have no azimuthal derivative. Multiplying by and using constant mass loading givesThus the magnetohydrodynamic angular-momentum invariant is constant along the line when . Let and define . Eliminating between the two invariants givesFor a highly sub-Alfvénic poloidal flow, , this is along a nonsingular field-line segment. This proves sub-Alfvénic isorotation in a steady axisymmetric wind, with the correction explicitly displayed. If the poloidal flow is exactly zero, the induction equation directly gives , namely Ferraro's law of isorotation. The approximate claim presumes regular invariants: small alone is not a uniform relative bound if is allowed to become arbitrarily large.
Matter corotating with the footpoint has fixed angular velocity . Its effective potential in that rotating frame is the sum of Newtonian gravitational potential and centrifugal potential,Along an outward-inclined straight magnetic field line, write and , where is distance from the footpoint. The exact potential along it isIts first derivative at is zero by the Keplerian rotation balance. At the footpoint the meridional Hessian is with zero mixed derivative. HenceWhen , the potential initially rises and a cold parcel must overcome a barrier. When , its quadratic curvature is negative, so the footpoint is a local maximum along the field and a small outward displacement is accelerated further outward:This is the thirty-degree magnetocentrifugal launching criterion. It describes the lack of a local cold-launch barrier, not a nonzero force on a parcel exactly at rest at . At exactly the quadratic term vanishes; for the specified straight line the next term is , as in marginal straight-line launch at thirty degrees. Global wind escape additionally depends on conditions farther along the line.
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