Use , and primes for derivatives. Time dependence is , so exponential growth means . The constant mass density and incompressible velocity give
All magnetic factors below use the source convention .
Linearizing the ideal magnetohydrodynamic momentum equation, the advective perturbation is . The magnetic force is , whose component vanishes. Thus the three component equations are
In particular the vertical equation has the pressure-gradient and magnetic signs printed in the PDF.
The incompressible ideal magnetohydrodynamic induction equation can be written . Linearizing it gives
For , these are
The term is essential: a perturbed vertical magnetic component is stretched by the background shear flow. Differentiating these amplitudes and using incompressibility also verifies .
For completeness, substitution into all three momentum equations gives
where is the vertical vorticity amplitude. Multiplying the equation by and subtracting times the equation eliminates pressure:
Therefore, away from ,
This is the nonresonant reduction relevant to the instability calculation. Division at the Alfvén wave resonance would be invalid. For a concrete counterexample to an unrestricted reading, take constant , , , and , with all other amplitudes zero. Every smooth solves the original linear system, but need not vanish. These transverse resonant waves do not drive . A genuinely growing mode in a real background has complex and cannot satisfy either or on the real axis. This explains exactly when the requested reductions may be used.
On that nonresonant branch, multiply the horizontal equations by and and add. Incompressibility gives , so
Combining incompressibility with vorticity, multiply its first equation by and subtract times the definition of . This gives
Consequently
Substitute this and the derivative of the displayed pressure relation into vertical momentum. Multiplication by gives
Expanding the second derivative once gives exactly the requested vertical-velocity equation:
To take the discontinuous-layer limit without multiplying distributions, introduce . It is proportional to the normal displacement: the material kinematic condition is , so . Since , . The same equation becomes the displacement equation for a parallel magnetic shear flow
The physical interface condition is continuity of , because both fluids move the same interface. For constant on each side, away from resonance the coefficient is constant and nonzero, so . Requiring decay at infinity and matching yields
The exponent is , as in the actual PDF; the converted TeX's there is a transcription error.
Integrate the conservative displacement equation across a layer of thickness . Its undifferentiated term has an integral tending to zero, while the derivative gives
Equivalently, the perturbed magnetohydrodynamic total pressure is and is continuous. With and , a nontrivial amplitude requires
This is also the rigorous thin-layer integration of the original vertical equation, after combining the derivative terms before taking the limit.
Put and . Completing the square gives the dispersion relation
For both interface frequencies are real, so there is no exponentially growing interface mode. Above that threshold, the growing sign has growth rate . This is magnetic stabilization of an equal-density vortex sheet: magnetic tension from bending the field overcomes the kinetic shear driving Kelvin-Helmholtz instability. Equality is marginal and the strict stable condition avoids its double-root degeneracy. The case has no streamwise shear drive and has the neutral interface frequency ; the nonzero-frequency elimination should be interpreted by the original equations or a limiting displacement formulation in that case. The horizontal affects the exponential decay length through , but not the stated threshold.
Use the adiabatic form of ideal magnetohydrodynamics: heat conduction and external heating are absent, so . Infinite electrical conductivity and zero viscosity alone would not remove the thermal source terms on the cover page. If those terms are retained, the energy equation below must acquire on its right-hand side.
Expanding the continuity equation gives its conservative form . Using it to expand the conservative momentum derivative gives
For , the Lorentz force density is the divergence of the magnetic Maxwell stress tensor:
Combining these identities with momentum balance proves
The dyadic stress contains both magnetic tension and magnetic pressure; the sign in the flux is fixed by moving the magnetic force to the left.
For the energy equation, first dot momentum balance with and add the adiabatic internal-energy equation. The continuity equation converts their material derivatives into conservative derivatives, while . The result is
The ideal magnetohydrodynamic induction equation gives the magnetic counterpart. In fact,
Thus the outward Poynting vector is , and magnetic work cancels the fluid work. Finally, the continuity equation implies
Adding all three identities gives ideal magnetohydrodynamic energy conservation in the required local form:
where
The magnetic energy coefficient is , as in the original PDF. For a self-consistent, time-dependent gravitational field this local balance should not be confused with a global self-gravitating energy integral: the latter uses gravitational field energy, or the familiar one-half factor in after the field is eliminated.
Work in the shock frame of a thin planar discontinuity, with normal speed . A smooth gravitational potential has no finite jump through a vanishingly thin front; its advected contribution cancels using the common mass flux. Integrating the conservation laws gives constant normal mass, momentum and energy fluxes, together with the normal-field and tangential-electric-field conditions of the ideal magnetohydrodynamic shock conditions.
For a parallel magnetohydrodynamic shock, and . The magnetic solenoidal constraint makes the same on both sides. The normal momentum flux is ; its magnetic term is therefore identical upstream and downstream. The Poynting vector is zero because . Hence the nontrivial jumps are exactly the Rankine-Hugoniot conditions for a perfect gas:
with specific enthalpy . Physically, motion along the straight field neither bends it nor compresses its transverse flux. The field consequently provides no changed stress or energy flux in this purely parallel geometry. This conclusion does not apply to a shock that develops a transverse magnetic field.
For a perpendicular magnetohydrodynamic shock, the magnetic field is tangential and the velocity normal. Steady induction makes continuous, while the continuity equation makes continuous. Dividing gives the magnetic flux freezing relation
Put , so and . Constant normal momentum flux now reads . Substitution gives
The magnetic correction is negative for compression: part of the incoming ram pressure builds magnetic pressure instead of thermal pressure.
Here the Poynting vector has normal component . Divide the constant energy flux by the nonzero mass flux to obtain
With , this gives the second expression for downstream pressure:
In this expression is the only downstream unknown. Equating the two pressure expressions and multiplying by yields
up to an overall minus sign, where and
The discarded factor is the unchanged state, not a compressive shock. This derives the polynomial for the compression ratio of a perpendicular magnetohydrodynamic shock without omitting its trivial branch.
For the usual physical adiabatic index , is strictly increasing for positive , has , and has one positive root. Since
that root is greater than one precisely when . The necessity is not limited to : for any , eliminating using gives
For , positive downstream pressure requires when . Moreover,
The bracket is positive throughout , even when . The exactly cold unmagnetized limit gives the familiar strong-shock upper compression ratio directly. Thus the physical compressive branch requires
The PDF's final denotes this same incoming speed . The right side is the squared speed of a perpendicular fast magnetosonic wave: the upstream flow must be super-fast-magnetosonic so that this compressive signal cannot run upstream against the incoming flow. At equality the shock amplitude vanishes into a characteristic disturbance.
Write . A fluid element in the homologous spherical flow obeys , so remains constant. Also . Along every element, the continuity equation therefore gives . Every element starts with the same mass density, and hence has the same mass density at subsequent times:
This proves preservation of uniformity, rather than assuming it when conserving the total mass.
By the shell theorem, only the mass interior to radius contributes to its gravitational acceleration. That mass is . The same result follows directly from the Poisson equation for Newtonian gravity: spherical symmetry gives , and regularity at the centre sets the integration constant to zero. Hence and
The material derivative of the background velocity is . There is no pressure force, and the momentum equation consequently reduces to
Multiplication by and integration, using collapse from rest, gives
Choose the negative square root for contraction. Put and . For , the energy integral then gives , while . Their ratio is
Integrating from the initial turning point proves the cycloid parametrization of pressureless homologous spherical collapse:
It covers the entire contracting branch, with complete collapse at and . At the uniform dust configuration is singular, so the smooth calculation is restricted to .
Each Fourier mode among the comoving perturbations of a homologously collapsing cloud has its phase fixed on each fluid element. In fact, for ,
Its physical wavelength contracts in proportion to , while its wavelength in the comoving coordinate stays fixed. This is the physical reason to use a time-dependent wavenumber; holding the physical wavenumber fixed would not follow the contracting pattern. Boundary effects are being excluded in this bulk Fourier mode calculation.
Let and let the perturbed velocity and Newtonian gravitational potential have amplitudes and . Linearizing the continuity equation, the uniform background eliminates . The advected phase eliminates its own time derivative, leaving
For the density contrast , use to obtain . The linear momentum equation and Poisson equation for Newtonian gravity are
Differentiating the density contrast equation must include :
Thus the compressive Fourier mode with satisfies
The pressureless approximation removes the usual acoustic restoring term of Jeans instability. A transverse velocity perturbation instead obeys and does not drive this density contrast.
Since , the density contrast equation becomes
For a direct verification, put . As , the first-derivative terms cancel, reducing the equation to
The function has second derivative and satisfies this equation. Transforming back gives the required growing branch:
To establish what the other solution does, use reduction of order, not just the growth of this example. The coefficient of is , so an independent solution is proportional to . Choose the integration endpoint at complete collapse to select the decaying branch:
For example, evaluating the integral with gives integrand and antiderivative . Its endpoint value gives the displayed expression. Its Wronskian with is , so the two solutions are independent on .
For , , and the integral in is . Consequently the two density modes of a collapsing pressureless sphere have
Equivalently, with , the local powers are and . There is one independent growing branch: every solution is , and only the branch with decays at collapse. The uniqueness is up to normalization and addition of the decaying solution; it does not mean that only one literal function can grow. A fixed nonzero initial perturbation will eventually violate , so the divergent linear result is not a nonlinear solution through collapse.
Figure 1.
Homogeneous collapse from rest and the growing and decaying fractional-density modes
. Details.

There are unlisted articles, also show them or only show them.