Write asDifferentiating twice, the moving-limit terms cancel at first order and yield at second order. Also and . Thus this integral operator is the inverse of with mixed Neumann boundary condition and Dirichlet boundary condition.
For , satisfies those conditions and . The corresponding mixed homogeneous equation has no nonzero solution, so uniqueness givesThis verifies the asserted eigenvalues and eigenfunctions for every .
Write using the Bessel function of the first kind. The wall boundary conditions at selectBecause , the sidewall no-penetration boundary condition requireswhere are the positive zeros of . These radial eigenfunctions automatically preserve layer volume becauseThe constant radial mode cannot change the interface height in a closed tank: the Laplace equation and the impermeable lids then give zero vertical velocity, and a uniform displacement would change each layer's volume.
The kinematic boundary condition fixesThus the interface values are and . Substitution in the normal stress condition gives the finite-depth Rayleigh-Taylor dispersion relation:soHere is the Atwood number. Every allowed mode has a positive growth rate and is subject to Rayleigh-Taylor instability. Since , shorter radial scales grow faster. The limits areThere is no fastest finite wavenumber in the ideal sharp-interface model without surface tension, viscosity or diffusion. The zero-initial-velocity condition uses both exponential branches: an initial mode evolves as . If the mass density ordering were reversed the same calculation would give oscillatory stable modes; equal mass densities give neutral modes.
For the linear differential operator , the exponential function is an eigenfunction: . Distinct give the two homogeneous solutions, while the method of undetermined coefficients supplies a particular solution at the distinct forcing exponent :
Past exam of the mathematics course of the University of Cambridge 2001 ib Paper 4 2H Solution Created 2026-09-24 Updated 2026-10-14
Differentiate the Legendre differential equation once and put :Multiplying by gives its Sturm-Liouville form,Thus the weight is , not one. For , is a nonzero polynomial; is a trivial solution rather than a nonzero eigenfunction.
Multiply the equations for by respectively, subtract and integrate. The resulting boundary term is , since all these derivatives are finite at the endpoints. For distinct nonnegative indices, , giving the weighted orthogonality of Legendre polynomial derivatives:For the integral is zero simply because .
Past exam of the mathematics course of the University of Cambridge 2001 iii Paper 54 3 Solution 2026-10-14
The spatial reflection acts on the two complex amplitudes as , because the first spatial eigenfunction is even and the second is odd. The first equation must therefore be even in , and the second odd. For a nonresonant double Hopf bifurcation, the temporal phases give independent actions , in the cubic normal form of a dynamical system. A cubic monomial in the first equation must have net phase weight one and net phase weight zero. Only satisfy this; the second equation similarly has . Parametrizing the independent cross-saturation coefficients givesAll coefficients can be complex: their real parts determine amplitude growth and their imaginary parts frequency shifts. These are cubic truncations of a family of reduced vector fields on the four-real-dimensional extended centre manifold, with the two unfolding parameters entering .
The nonresonance assumption must be made explicit. Merely having does not imply this form: for , the quadratic terms in and in satisfy both temporal resonance and spatial parity. Thus the initial form is the generic nonresonant double-Hopf form, rather than a statement for every possible unequal frequency pair.
At the one-to-one reflection-symmetric one-to-one Hopf resonance, only the common temporal phase action remains. Cubic terms must then have total phase weight one. Spatial reflection retains, in the first equation, the three terms ; the second retains . Common phase covariance excludes all quadratic terms. The additional resonant terms are consequently and , with independent complex coefficients. This is the reflection-symmetric one-to-one Hopf resonance.
In the specified equal-coefficient specialization, put . A nonzero pure- periodic branch exists for and hasIts radial eigenvalue is , and its phase is neutral. For a transverse perturbation the linear equation isIts time dependence can be removed exactly by . Using and givesWriting , , yields the constant real stability matrixLet . The transverse characteristic polynomial isBoth transverse eigenvalues have negative real part exactly whenThese hold at because . Thus a sufficiently small pure branch is transversely stable; it is stable modulo its neutral temporal phase until one of the two inequalities fails. The secondary steady and Hopf thresholds of a resonant pure mode are derived in the two parts below. They refer to accessible points on the pure branch; in a multi-parameter problem may also vary, so a proposed parameter path must actually cross the corresponding surface.
Past exam of the mathematics course of the University of Cambridge 2001 iii Paper 57 2 a Solution Created 2026-10-03 Updated 2026-10-14
For admissible initial data, for example a square-integrable function on the interval, expand in the sine eigenfunctions of the Dirichlet Laplacian:The expansion follows either from separation of variables or the complete sine orthogonal basis. If , every growth rate is negative and Parseval's identity givesThus all finite-energy data decay. The convergence is also uniform in after any fixed positive time: apply Cauchy-Schwarz inequality to the sine series, using the summable factors , to bound its supremum by a constant times for .
Conversely choose . Then , which is stationary at equality and grows when . All initial conditions decay if and only if . This is the continuous part of the reaction-diffusion spectral decay threshold.
Past exam of the mathematics course of the University of Cambridge 2002 ib Paper 2 9D Solution Created 2026-09-24 Updated 2026-10-14
Use the position-space momentum operator and set . Direct differentiation givesTo compute the squared orbital angular momentum, write , , , so . Expanding the products, including derivatives of their variable coefficients, givesFor example ; summing the three cyclic expressions proves the identity.
Here and , so . ThereforeThis is the angular momentum of a homogeneous harmonic polynomial, with angular quantum numbers . The polynomial is a nonzero angular eigenfunction; by itself it is not a normalizable full-space wavefunction.
Past exam of the mathematics course of the University of Cambridge 2002 ib Paper 3 12A Solution Created 2026-09-24 Updated 2026-10-14
Use the weighted inner product . For real eigenfunctions, integration by parts with the zero endpoint values givesThus . The regular separated Sturm-Liouville problem has simple eigenvalues: for a fixed eigenvalue, prescribing leaves only the initial flux free, so uniqueness of the associated first-order system makes any two eigenfunctions proportional. Distinct eigenfunctions are therefore orthogonal, and choosing their signs and scales so that givesThe positive energy form realizes as a positive self-adjoint operator in this weighted space, with compact inverse on the bounded interval. The spectral theorem for compact self-adjoint operators supplies a complete eigenbasis. This is the standard regular Sturm-Liouville eigenfunction expansion, also valid with continuous by working with the continuous flux .
For a source , expand a zero-endpoint solution of in that basis. Multiplication by and unweighted integration giveSince is not an eigenvalue, every coefficient is determined. The spectral Green function of a regular Sturm-Liouville problem is consequentlyWeighted completeness means as a distribution, so applying to this series produces the required delta source. The source integration is with , explaining the absence of an additional factor in the stated kernel.
For the subsequent operator the sign is explicitly reversed: and . To cover every real non-eigenvalue , define the homogeneous solutionIt satisfies , and . Matching the two endpoint solutions continuously at with derivative jump yieldsThe denominator is nonzero precisely off the Dirichlet eigenvalues . In particular . At , its spectral expansion givesThis odd reciprocal-square sum from a Dirichlet Green function proves .
Past exam of the mathematics course of the University of Cambridge 2002 iii Paper 49 2 Solution Created 2026-10-03 Updated 2026-10-14
Let be layer thickness and gravitational acceleration. The unforced shallow water equations on the equatorial beta plane areLinearize about , . Put and , and scale , , and . Dropping capitals, the linearized shallow water equations becomeThe choice makes both the wave speed and the coefficient of the dimensionless Coriolis parameter equal to one.
Take Fourier modes that decay as . Their equations areFor and nonzero , the first two require . The root gives , and meridional balance becomes . Hence the equatorial Kelvin wave isIt travels eastward at speed in dimensional units. The other sign gives and , so is not trapped.
For , and , inversion of the first two equations gives the equatorial wave velocity polarizationSubstitute in the remaining momentum equation. Multiplication by leavessoWriting yields , the Hermite differential equation. The trapped solutions have the Hermite oscillator quantization and .
For completeness, quantization follows without assuming that every acceptable solution is a polynomial. On decaying smooth functions, define , and . Integration by parts gives and . If , it is an eigenfunction of with eigenvalue . Repeated lowering must terminate: otherwise it eventually produces an eigenvalue below one. At termination , so the terminal eigenfunction is and has eigenvalue one. Repeated raising gives and ; uniqueness of a decaying solution at one end of this second-order equation fixes each mode up to scale.
Thus, away from the exceptional quotients, all fields are determined byInsert this and its derivative in the polarization formulae to obtain and . For , the cubic supplies the low-frequency equatorial Rossby wave and two equatorial inertia--gravity wave branches. Their meridional structures are Gaussian-weighted Hermite polynomials.
For , multiplication by factorizes the equatorial shallow-water dispersion relation asThe physically admissible quadratic gives the mixed Rossby-gravity wave, equivalently the Yanai wave:These fields satisfy all three original equations directly and decay at both infinities, including where the quotient formulae are singular.
To test the other factor, set . The original equations give and . Put ; meridional momentum then givesDecay of at both infinities requires the integral of the right side to vanish. Hence unless . Ordinarily the extra factor supplies no trapped mode. At the exceptional root of the mixed Rossby-gravity mode, , it coincides with the quadratic root and gives the same physical fields, not an additional branch. This distinction avoids discarding a regular physical mode at the crossing.
These arguments concern nonzero wave angular frequency. At , the oscillatory nonzero- modes have , while zero-frequency geostrophic states must be considered in the original equations rather than in expressions divided by .
Past exam of the mathematics course of the University of Cambridge 2002 iii Paper 58 1 ii Solution Created 2026-10-03 Updated 2026-10-14
At the double threshold, . For , , so and every remaining eigenvalue is strictly negative. There is a spectral gap separating this two-dimensional kernel from the stable modes. The centre manifold theorem therefore gives a two-dimensional state centre manifold, withIf the two detuning parameters are adjoined as variables with zero time derivatives, the extended centre manifold has total dimension four; its state fibers still have dimension two.
The only nontrivial spatial symmetry of the bounded interval is the reflection . Since is even and odd, its group action on the amplitudes is . Thus equivariance requires to be even and odd in . There is no sign symmetry , because the quadratic nonlinearity breaks it. The general smooth form is , , with the zero solution preserved. The quadratic even-odd mode interaction follows on truncation:Writing and , the exact linear growth rates are and . To first order in detuning,The orthogonal projection of the quadratic term onto the neutral eigenfunctions determines the leading coefficients. Both eigenfunctions have squared norm one, and parity kills the unwanted products. The quadratic correction contributes no term through , since is self-adjoint and the projected modes lie in its kernel. ConsequentlyThese projections are also a concrete way of computing the normal form. In this normalization they give , and , consistent with the stated coefficient ratios.
Past exam of the mathematics course of the University of Cambridge 2002 iii Paper 58 1 i Solution Created 2026-10-03 Updated 2026-10-14
The linearization at the zero solution is the self-adjoint differential operator , with domain satisfying both endpoint conditions. The Dirichlet boundary condition for on gives the orthogonal eigenfunctions and . Their second derivatives are multiples of themselves, so the additional condition is automatic. Completeness of the Dirichlet eigenfunctions also shows that these exhaust the spectrum of the polynomial operator . Set ; each eigenfunction has growth rate . Hence the stationary bifurcation thresholds areEquality of the first two thresholds requires to be the midpoint of and , since these numbers are distinct. ThereforeAt this point the even and odd lowest eigenfunctions become neutral simultaneously.
Past exam of the mathematics course of the University of Cambridge 2004 ib Paper 1 19D Solution Created 2026-09-24 Updated 2026-10-14
The angular momentum commutation relations are . The commutator product rule givessince the bracketed expression is symmetric in and is antisymmetric. Alsoproving .
For orbital angular momentum, . A differentiable radial function has , so its contraction with the antisymmetric symbol vanishes: . Put . The coordinate differential operators give , whileannihilates every power of , because . Since all annihilate the radial factor, the product rule yieldsSubstitution into the expression for gives the highest-weight complex-coordinate orbital wavefunction resultAs , lowering preserves this eigenvalue whenever the lowered function is nonzero. Explicitly,For the lowered function is zero, so it is not an eigenfunction. For the original nonzero function has the usual regular angular dependence. The PDF's “any integer” differential identities also hold locally for negative where , but those negative powers are singular on the axis and are not square-integrable regular angular eigenstates. The converted TeX incorrectly writes in place of the PDF's .
Past exam of the mathematics course of the University of Cambridge 2004 iii Paper 64 2 Solution Created 2026-10-03 Updated 2026-10-14
The equilibrium isothermal equation of state is . Hydrostatic equilibrium gives , henceHere is assumed. This is the same local harmonic-gravity balance as isothermal vertical structure in stellar gravity.
For , this equilibrium is stably stratified under adiabatic fluid perturbations. Its squared buoyancy frequency isA general perturbation can therefore support acoustic waves restored by compression and internal gravity waves restored by buoyancy, with nonoscillatory entropy or vortical disturbances also possible. The prescribed velocity is purely vertical and horizontally uniform. It describes vertical acoustic waves; it does not contain the horizontally varying circulation required for an oscillatory internal-gravity branch. For zero horizontal wavenumber, that branch has zero frequency. An isothermal equilibrium must not be confused with an isothermal perturbation: the latter would remove the buoyancy restoring force.
Introduce the fluid Lagrangian displacement , so . Use for fluid Eulerian perturbations and for fluid Lagrangian perturbations. The continuity equation and the adiabatic relation areThe fixed external gravitational potential is not perturbed. The vertical linearized Euler equations consequently giveSubstituting the preceding relations, and using and , reduces its right-hand side toSince and , the same equation holds for :The rigid fixed base supplies the essential condition . At infinity the condition is finite kinetic energy, not bounded velocity amplitude; a polynomial can grow while the Gaussian mass density makes its energy finite.
Put and . The equation becomes the Hermite differential equation in its probabilists' convention,For , its recurrence isThe base condition makes and therefore every even coefficient zero. An odd series terminates at degree when . It remains to prove that a nonterminating odd solution cannot have finite energy; termination alone would not establish the requested exhaustion of modes.
For that purpose, set . The finite-energy condition is , and its equation isBecause the coefficients are even and the solution is odd at the base, extend oddly to the whole real line. Define lowering and raising operatorsIntegration by parts gives , so . These identities apply to the square-integrable solution: multiplying its equation by a compactly cut off conjugate and taking larger cutoffs bounds and in , and removes the endpoint terms. The same argument applies to each lowered eigenfunction.
If is not a nonnegative integer, repeatedly apply . Each application lowers by one and remains nonzero whenever its current value is positive, by the norm identity. After finitely many applications it would yield a nonzero square-integrable eigenfunction with negative , contradicting that identity. Thus is a nonnegative integer. At , gives , which is even. Lowering reverses parity, so an initially odd eigenfunction can reach this even ground state only if is odd. Consequently . The recurrence then terminates and uniquely determines the odd solution from .
The complete adiabatic vertical modes of a Gaussian atmosphere are thereforeHere is the Probabilists' Hermite polynomial. For example the first shapes are , , and , with frequencies squared , , and . Either sign of each real frequency gives a time-harmonic solution. Gaussian moments make every displayed polynomial have finite kinetic energy. Without the fixed-base condition, finite energy alone would also admit even polynomials, which is why that condition is necessary.
Past exam of the mathematics course of the University of Cambridge 2005 ia Paper 2 6B Solution Created 2026-09-24 Updated 2026-10-14
Substitution of the power series, with termwise differentiation, gives the coefficient identityThus and are arbitrary, and all power series solutions of the Hermite differential equation areAn empty product is one. For a nonterminating branch the ratio of consecutive terms in its own parity subsequence is asymptotic to , hence tends to zero for every fixed . The ratio test proves convergence everywhere; the resulting power series can be differentiated termwise and indeed solve the differential equation. A terminating branch is already a polynomial.
The boundary condition forces ; the solution is odd. Apart from the zero solution, which works for every , a polynomial occurs exactly when an odd index satisfies . Before that index the odd coefficients are nonzero, and after it they vanish. Thus the odd polynomial solutions of the Hermite differential equation haveEquivalently, comparison of leading polynomial coefficients gives , proving that no other nonzero polynomial is possible. Normalizing by , the polynomials of degree below six areEach can be multiplied by an arbitrary nonzero constant; these are normalized odd Hermite polynomials.
Let . The forcing in the final inhomogeneous linear differential equation is precisely the displayed degree-five eigenfunction , with . HenceDirect differentiation gives , and . Among polynomial solutions this choice is unique: a polynomial in the kernel of must be constant, and its value at zero eliminates that constant.
Past exam of the mathematics course of the University of Cambridge 2005 iii Paper 20 1 Solution Created 2026-10-03 Updated 2026-10-14
The central problem of spectral geometry is how much of a Riemannian metric is determined by the eigenvalues, with multiplicities, of its Laplace-Beltrami operator. For a membrane with fixed boundary, the squared vibration frequencies are proportional to the Dirichlet eigenvalues. Kac's 1966 paper brought this inverse problem into focus: the full sequence of frequencies might encode a domain's shape, but recovering a few geometric quantities is much weaker than recovering an isometry class.
The first major line of development extracts geometric information from spectral sums. On a smooth closed -dimensional manifold, the heat trace has the short-time expansionwhere are the nonnegative eigenvalues of and is scalar curvature. The coefficients are heat invariants, formed by integrating local curvature expressions. They recover dimension, Riemannian volume and total scalar curvature. For smooth planar domains with the Dirichlet boundary condition,Thus area and boundary length are audible. The constant term also contains topological information through Gauss-Bonnet theorem, with corner corrections when the boundary is polygonal. The Weyl law is the corresponding leading eigenvalue-counting result. Neither the leading term nor the whole list of local heat coefficients automatically reconstructs global geometry.
In the 1970s, the wave trace introduced a complementary link with global closed geodesics. The distributionis spectral, while its singularities are governed by periodic geodesic motion. The 1975 Duistermaat-Guillemin work made this relationship precise. Its trace formula places singularities at geodesic lengths and computes their coefficients under suitable clean or nondegenerate hypotheses. When a coefficient is nonzero, the corresponding length is audible. Possible cancellation must be addressed before identifying the entire length spectrum with the singular support. This approach led to spectral rigidity questions, rather than just the recovery of integral curvature quantities.
The second main line constructs counterexamples to metric determination. A precedent was the 1964 flat-torus example: different sixteen-dimensional Euclidean lattices could give the same Laplacian eigenvalues. Subsequent lattice constructions lowered the dimension; Conway and Sloane's 1992 work exhibited four-dimensional Euclidean lattices with matching lattice theta series. For a flat torus , the spectrum is the multiset for , so equality of lattice theta series of the dual lattices gives isospectrality even when the Euclidean lattices are not related by an orthogonal transformation.
A systematic geometric construction arrived with the Sunada theorem in 1985. For a common Riemannian cover with finite isometry group , almost conjugate subgroups have the same number of invariant vectors in each Laplacian eigenspace. Their freely acting quotients are therefore isospectral manifolds. This reduces an analytic equality to a finite-group representation identity. It produces many examples on surfaces and in higher dimensions, but nonconjugacy of the subgroups must be supplemented by an argument excluding extra quotient isometries. Transplantation theorem provides an explicit version: piecewise eigenfunctions are recombined by a fixed invertible linear transformation that respects the gluing and boundary conditions.
The planar problem itself was answered negatively by Gordon, Webb and Wolpert in 1992: noncongruent simply connected polygonal plane domains have equal Dirichlet spectra. This is stronger than counterexamples among abstract manifolds or flat tori, since these are genuine two-dimensional planar membranes. It does not settle every restricted version, such as asking for two domains within a specified smooth or convex class.
By the 1990s, isospectrality was also known to coexist with continuous metric variation and changes in local geometry. For example, a 1997 construction gives continuous isospectral families on products of spheres and tori whose members need not be locally isometric; in some examples the maximum scalar curvature changes. Conversely, rigidity and compactness results show that an isospectral class is not unrestricted. The 1988 surface compactness theorem makes fixed-spectrum sets of closed orientable surface metrics compact modulo diffeomorphisms. Compactness does not mean there is only one metric, or even finitely many metrics. By 2005, the subject therefore combined local heat invariants, global geodesic information, group-theoretic constructions, explicit transplantation and geometric rigidity. The spectrum determines substantial geometry, while generally failing to determine the full metric.
Past exam of the mathematics course of the University of Cambridge 2005 iii Paper 20 2 Solution Created 2026-10-03 Updated 2026-10-14
For a smooth function and the Levi-Civita connection , the Riemannian Hessian is the covariant two-tensorThe connection rules show that this is linear over smooth functions in both vector-field arguments, so it is a tensor. Torsion-freeness gives its symmetry:Its metric trace defines the paper's Laplace-Beltrami operator, ; its eigenvalues on a closed manifold are nonpositive. We use when listing nonnegative eigenvalues or writing .
At , choose an orthonormal basis of the tangent space and unit-speed geodesics . Differentiating twice along a curve givesThe covariant acceleration vanishes on a geodesic. Taking the trace at proves the geodesic trace formula for the Laplace-Beltrami operator:The last equality is Taylor's formula along the geodesics, and expresses the Laplacian entirely through nearby function values.
For stabilization, let be the assumed isospectral nonisometric four-dimensional tori, and let . Take the same small flat torus as an extra factor. On a Riemannian product,If and are eigenfunctions with eigenvalues and , then has eigenvalue . Products of orthonormal eigenbases are complete in the product space, so this lists all eigenvalues with multiplicities, including coincidences between different sums. Consequently the two products are isospectral.
One must also prove that multiplying by a common factor has not accidentally made the two manifolds isometric. ChooseThe injectivity radii are positive because the factors are compact. A closed product geodesic of length less than projects to a closed geodesic of length less than in . Such a projected geodesic must be constant: otherwise its initial vector over one period would be a nonzero vector of norm below the injectivity radius mapping back to its starting point under the exponential map. Thus all sufficiently short closed geodesics lie in the directions. Conversely the coordinate circles, of length , pass through every point and span those directions.
It follows that the smooth distribution tangent to the small flat-torus factor is characterized intrinsically by the span of tangent vectors to closed geodesics of length below . A hypothetical product isometry would preserve this smooth distribution and its orthogonal complement. The latter has leaves ; the isometry and its inverse take whole leaves to whole leaves, thereby giving an isometry , a contradiction. This proves isospectral stabilization by a small flat torus:This argument works even without assuming that the original four-dimensional torus metrics are flat.
Past exam of the mathematics course of the University of Cambridge 2005 iii Paper 20 3 Solution Created 2026-10-03 Updated 2026-10-14
Work on a closed compact smooth Riemannian manifold without boundary, as in the usual discrete spectral setting here. Use the paper's , and put . The Riemannian heat kernel is the smooth kernel, for , representing the solution ofThus and its distributional initial value in is the Dirac delta distribution at . The heat trace isThe heat invariants are the coefficients in the short-time heat trace expansion specified below.
To derive its spectral form, take an orthonormal eigenbasis , with , repeating eigenvalues according to multiplicity. For the initial datum , the function solves the heat equation. Uniqueness identifies it with the heat-kernel solution. Expanding arbitrary initial data in this basis therefore gives the spectral expansion of the Riemannian heat kernel:Standard elliptic estimates and eigenvalue growth imply smooth convergence for bounded away from zero: polynomial bounds on derivatives of eigenfunctions are dominated by the exponential factors. On the diagonal all summands are nonnegative, so monotone convergence also justifies integration without needing an interchange of conditionally convergent terms. Since each eigenfunction has unit norm,Equivalently, if the paper's Laplacian eigenvalues are written , the formula is ; a growing exponential is not the heat semigroup.
Here are the needed heat kernel expansion facts, stated without proof. On a closed -dimensional smooth Riemannian manifold,with the diagonal remainder uniform in after any finite truncation. The coefficients are smooth local geometric quantities; . Compactness therefore allows integration term by term:These integrated coefficients are the heat invariants. The uniform leading remainder in particular gives .
Isospectral manifolds have identical heat traces by the derived spectral formula. If their dimensions were , multiplying the common trace by would give a finite positive limit on the -dimensional manifold but divergence on the -dimensional one. Thus the dimensions are equal, and equality of the leading coefficient gives equal Riemannian volume. Explicitly,The absence of a boundary fixes this particular integer-power expansion. With a boundary one must first specify boundary conditions and include the appropriate half-integer boundary terms; the leading dimension-and-volume conclusion remains valid in the usual compact smooth setting.
Past exam of the mathematics course of the University of Cambridge 2005 iii Paper 67 1 e Solution Created 2026-10-03 Updated 2026-10-14
Expanding the matrix determinant from part (b) givesThe finite-interval Airy spectral determinant obeys . At the origin,This zero comes from coalescence of the three rotated equations; it is removable in the underlying boundary system. Indeed, with has only the zero quadratic solution.
For , a zero of is equivalent to the existence of a nonzero combination satisfying the homogeneous endpoint conditions. This can be checked by expanding the determinant of those three endpoint equations. Such a function satisfies , so it is an eigenfunction of with eigenvalue . Integration by parts yieldsso every nonzero zero has . None lies on the boundary : by a cube-root rotation it suffices to take real. With , the determinant equation becomesThe right-hand side has squared modulus for , whereas the left-hand side has modulus one. Therefore there are no nonremovable spectral poles in , and the contour representation has no discrete residue contribution from that domain.
Taken literally as a claim about the operator's discrete spectrum, however, the printed assertion is false. To see this constructively, put , . ThenThus zeros occur whenBetween successive positive cosine maxima and adjacent negative minima the difference changes sign. There are consequently infinitely many positive roots, producing genuine negative eigenvalues of . The third-order resolvent maps into , whose inclusion into is compact, so these are indeed discrete spectrum of an operator with compact resolvent. The valid conclusion is absence of poles in the reconstruction sectors, not absence of operator eigenvalues.
Past exam of the mathematics course of the University of Cambridge 2005 iii Paper 71 2 Solution Created 2026-10-03 Updated 2026-10-14
Linearizing the ideal magnetohydrodynamic induction equation about a static magnetic field and using gives the fluid Lagrangian displacement-generated magnetic field perturbation . The two solenoidal vector field conditions reduce the curl identity toIts divergence vanishes because it is a curl. Directly, the two products of first derivatives in cancel after exchanging their indices, while the remaining terms differentiate or , both zero. Similarly the integrated linear continuity equation gives , so .
Let be the magnetohydrodynamic total pressure. Magnetostatic equilibrium and the momentum equation in the linearized ideal magnetohydrodynamic equations areThere is no perturbed gravitational potential here because the field is fixed. Multiply by and integrate. The pressure term vanishes by the assumed boundary cancellation and . Thuswhere .
Integrate the first magnetic term along , using , then insert the expression for . This gives the positive term and two mixed derivative terms. For clarity, the troublesome term transforms asThe first term on the right cancels the other mixed term. Combining the remaining derivative with the term containing givesDifferentiating the equilibrium relation now combines the gradient of mass density and magnetostatic equilibrium terms:We obtain the incompressible magnetic displacement energy identityThe two Hessian matrices are real symmetric, making their Hermitian form evaluations real. The last term is a squared norm, and for a nonzero displacement in fluid with positive mass density. Thus . It may be negative, in which case one temporal branch has exponential growth; real squared frequency is not itself a proof of stability.
For the atmosphere with a horizontal magnetic field, has zero Hessian matrix and the equilibrium equation isConsequently the interchange stability of an incompressible magnetized atmosphere is governed by the numeratorFor , the magnetic tension term is zero: these fluid Lagrangian displacements interchange neighboring magnetic field lines without varying along them. A mass density increasing with height gives negative energy and instability; decreasing mass density gives positive energy for these vertical interchanges. If everywhere, the displayed form is nonnegative for every admitted incompressible displacement. If the gradient changes sign, suitably localized divergence-free interchange trials detect an unstable inverted layer; For example, take and , with supported in that layer. Their divergence is zero, and neither component varies along the magnetic field.
For , magnetic field lines are bent. Averaging over a full horizontal wavelength gives the trial Rayleigh quotientunder the stipulated admissible boundary/integrability conditions. It is a trial quotient, not a claim that this displacement is an exact eigenfunction for every profile. mass density decreasing upward is stable here too. For inverted mass density, magnetic tension can stabilize sufficiently short waves along the magnetic field, but does not remove the transverse interchange instability. Locally the two contributions have the familiar scale , with the Alfvén speed .
Past exam of the mathematics course of the University of Cambridge 2005 iii Paper 79 4 b Solution Created 2026-10-03 Updated 2026-10-14
First assume the usual diffusion regime , with real; the complex-diffusion extension is described below. Substitution of a global normal mode givesSet to remove the first derivative, then put . The resulting oscillator equation isWriting gives the Hermite differential equation, . For a power series , its recurrence isTermination at degree requires . If it does not terminate in the appropriate parity, the series has a growing Gaussian component at one infinity; the solution decaying at one end then fails at the other. The Hermite oscillator quantization can also be seen from the self-adjoint operator , whose square-integrable eigenfunctions are the Hermite functions. Their spectrum is with . The ground state shows that the paper's phrase “positive integer” must include zero.
The global modes of a quadratically confined Ginzburg-Landau equation are thereforeTheir spatial functions are proportional to ; the quadratic Gaussian decay dominates the linear drift factor at both infinities. For real coefficients, the most dangerous mode is . The system has global hydrodynamic instability precisely whenEquality is marginal and smaller gives decay of all these modes. The finite-width confinement correction explains why a locally absolutely unstable region need not immediately support a growing global mode.
If complex diffusion is intended, impose the parabolic condition and choose with positive real part. The same formulas continue along the rotated ray, with the corresponding branch of ; instability is determined by the real part of the square bracket. Arbitrary constant , especially negative diffusion, does not justify the asserted whole-line Hermite decay or a well-posed evolution.