Backward-sign Airy half-line global relation 2026-10-14
For the Airy equation with opposite dispersive sign, on , let be the initial Half-range Fourier transform and . Three integrations by parts give the displayed global relation. The spatial transform is holomorphic for , whereas the finite-time spectral boundary transforms are entire functions. The symmetry , , preserves their time exponent.
// Target: analysis.bigb
Fluid-loaded membrane edge scattering Created 2026-10-06 Updated 2026-10-07
A pinned semi-infinite membrane scatters an incoming guided mode into reflected guided modes and outgoing sound. For unit incident displacement the scattered endpoint value is . Its Half-range Fourier transform therefore has nonzero endpoint terms even though the total displacement vanishes. The Wiener-Hopf equation kernel is with the outgoing branch .
For , an exponential gauge removes the second derivative. With and , the remaining equation is . Negative improves spatial decay of the transformed initial data; positive can destroy the convergence of its Half-range Fourier transform.
Half-line drift global relation 2026-10-06
For the advection-diffusion equation on , the spectral divergence form uses and factor . With negative-exponential Half-range Fourier transforms, integration gives the displayed global relation for . The boundary transform refers to , the negative of the outward normal derivative.
For the linear dispersive Stokes equation , let . Its local relation is obtained with . Integrating over the half-line gives the displayed global relation, with negative-exponential Half-range Fourier transforms and . The spatial transforms are holomorphic for , whereas the finite-time boundary transforms are entire functions.
Past exam of the mathematics course of the University of Cambridge 2003 iii Paper 61 1 b Solution Created 2026-10-03 Updated 2026-10-14
Use the Half-range Fourier transform and the finite-time spectral boundary transformswhere for . The spatial transforms are holomorphic in , while these finite-time transforms are entire functions. For now is an unknown boundary trace. Integrating the local relation over the half-strip, using spatial decay at infinity, gives the global relationThe boundary sign follows from integrating the flux derivative: its contribution is minus the flux at zero.
Fourier inversion first gives the initial real-line integral plus a real-line integral of . To put the boundary contribution on its useful complex contour, defineOrient its full boundary with on the left. It consists of the real axis from left to right and the upper curve from right to left. The real-axis piece must not be discarded for this dispersion. The contour integration representation isTo justify the replacement, the integral of along is zero by closing above . In that region , and each boundary term is an integral of over times a polynomial in . This has no growing temporal exponential there; suppresses the upper closing arc for . The Cauchy integral theorem then applies. The figure shows the full contour and, separately, the sectors used in the nonlinear problem.
Full cubic-dispersion contour and bounded-column sectors for reverse-dispersion mKdV
. Details. One may replace by for any finite . Their difference is a future-time integral over ; its factor decays inside , so its integral around vanishes. All contour formulas are understood as limits of truncated contours, with standard small displacements if a boundary transform needs an Abel limit. Compatibility of the initial and boundary data controls the corner behavior. This is the two-trace half-line cubic dispersion representation.
Past exam of the mathematics course of the University of Cambridge 2003 iii Paper 74 1 Solution Created 2026-10-03 Updated 2026-10-14
Fluid-loaded plate. Use complex amplitudes with time dependence and take the velocity potential in the fluid above the elastic plate to be . Let and be the undisturbed mass density and speed of sound. The linearized Euler equations give ; the kinematic boundary condition is . We model loading from one fluid half-space, with no fluid loading on the other face. Loading by identical fluids on both faces instead doubles the fluid term below.
Define the Fourier transform and its inverse byThe Sommerfeld radiation condition selects , with and . Here and in the diffraction calculation below, the outgoing square root is specified by first taking . Draw a vertical cut upwards from and another downwards from , and putThus is analytic in the upper half-plane and in the lower half-plane. In the real-frequency limit,The Fourier transform contour follows the real axis with the limiting-absorption pole prescriptions. In particular, an outgoing propagating component has positive vertical wavenumber.
The kinematic boundary condition gives , so . Eliminating the fluid pressure from the bending balance gives the line-forced fluid-loaded bending plate kernelFor harmonic line force amplitude at the origin, the plate displacement and fluid velocity potential are thereforeAn arbitrary localized loading replaces by its Fourier transform. This representation both calculates the response and identifies its different wave components through poles and branch points.
For an observer , , with , the method of steepest descent uses the saddle point . At fixed angle away from grazing, the acoustic far field isThe spreading is that of cylindrical acoustic waves. The phase velocity parallel to the plate is : components with are supersonic in that sense and radiate, whereas those with are subsonic and exponentially decay normally to the plate. The latter have reactive fluid loading and zero mean normal acoustic energy flux.
There is also a real guided root . Indeed, , , andThe residue theorem then gives an outgoing displacement contribution . It transports energy along the plate while its fluid field decays as . Other zeros on continued sheets can describe leaky or resonant waves; branch point contributions describe near and grazing fields. A fixed-angle acoustic far field expansion is not uniform near the plate, where these components can matter.
For a propagating spectral component, write . Its upward normal velocity is and its pressure is . Applying Parseval's identity to the time-averaged acoustic energy flux gives the upward power per unit length of the forcing line:Equivalently, the integrand is with prefactor . Integrating the radial acoustic intensity of the far field over a semicircle gives the same expression. The input power also feeds guided waves along the plate, so it must not be identified with alone.
Rigid half-plane diffraction. Suppress the time factor and assume . Write , , and denote the incident spatial field by . The Helmholtz equation, Sommerfeld radiation condition, and square-root branches are as above. Across the open positive axis the scattered field and its normal derivative are continuous. Across the rigid negative axis its normal derivative is also continuous, while its potential can jump. Let be this jump, supported on . The transformed scattered field isThe jump transform is analytic in the upper half-plane. The absence of an even scattered component follows from derivative continuity and the outgoing condition. Its normal derivative on either face is .
On the negative axis this derivative must cancel . Since the Half-range Fourier transform of is , the Wiener-Hopf equation has the formwhere is the transform of an unknown function supported on and analytic in the lower half-plane. The incident pole lies below the Fourier contour. Divide by and perform pole subtraction in a Wiener-Hopf equation:The first term is upper analytic and the second lower analytic, since the latter's apparent pole cancels. Equality of the two continued sides gives an entire function. The finite-energy edge condition, with , and the decay of the transforms at infinity force that function to vanish by Liouville's theorem. ConsequentlyThis is the Wiener-Hopf solution of rigid half-plane diffraction with the present transform and time conventions.
Deforming to a steepest descent contour gives a residue from the incident pole precisely when . At that pole ; its residue producesThus the total geometrical optics field is plus a reflected wave in the upper reflection region; in the lower shadow region the scattered residue cancels , and outside that shadow the direct incident wave remains. This gives both the amplitude and the spatial support of the geometrical optics fields rather than merely naming a reflected wave.
For , , , the saddle contribution uses and . The diffracted wave isThe total field is to this order. This far-field expression applies away from the shadow/reflection boundaries . There the pole and saddle coalesce, and a uniform Fresnel integral approximation replaces the divergent separate terms by a smooth transition. The exact contour integral remains well defined.
Past exam of the mathematics course of the University of Cambridge 2004 iii Paper 61 1 a Solution Created 2026-10-03 Updated 2026-10-14
Set , , and use the gauge reduction of a third-order half-line equationThe spatial differential operator acting on is obtained by replacing with . Its second-derivative coefficient vanishes. The first-derivative coefficient is , and the constant coefficient is . The time derivative supplies , so all constant terms cancel and the remaining equation is .
The transformed initial condition and Dirichlet boundary data are thereforeCompatibility at the corner is preserved. Since , this exponential gauge improves the spatial decay of the initial data, which supports convergence of its Half-range Fourier transform.
Past exam of the mathematics course of the University of Cambridge 2004 iii Paper 61 1 c Solution Created 2026-10-03 Updated 2026-10-14
Use the negative-exponential Half-range Fourier transformFor the boundary traces , define finite-time spectral boundary transforms . Integrating the conservation law in and then time gives the global relationThe plus sign of the boundary contribution follows because the integrated flux is .
Fourier inversion consequently gives a real-line initial integral plus a boundary integral. To put the latter in the complex plane, defineOrient from the left upper infinity, through , to the right upper infinity, with on the left. Each is entire, and in the region between the real axis and this contour, . The causal factors are bounded there and decays for . The Cauchy integral theorem, with the usual large-arc limiting argument, deforms the boundary integral to giveInitial smoothness, spatial decay and corner compatibility justify inversion; if necessary the integrals are first regularized before contour deformation. The unknown Neumann-type traces will be removed by the global relation.
Past exam of the mathematics course of the University of Cambridge 2004 iii Paper 61 1 f Solution Created 2026-10-03 Updated 2026-10-14
The algebraic change of variables still works for , but the transformed initial data are now multiplied by . Mere decay of does not ensure existence of the Half-range Fourier transform used above. For example, with gives a growing transformed profile.
There is also a genuine stability distinction. On the whole line a real-frequency mode of the original equation evolves with factorIts modulus is , so positive amplifies arbitrarily high frequencies rather than damping them. Thus the formal gauge equivalence does not justify the same unweighted Sobolev well-posedness conclusion. Weighted or more strongly decaying data and corresponding contour changes may allow particular solutions; the assumptions stated for the negative- construction cannot simply be reused.
Past exam of the mathematics course of the University of Cambridge 2006 iii Paper 86 1 a Solution Created 2026-10-03 Updated 2026-10-14
Extend by zero to the negative half-line. Its ordinary Fourier transform is then exactly the Half-range Fourier transform . The Fourier inversion theorem gives the real-line term for ; no endpoint convention at is needed.
It remains to show that each extra contour contributes zero, independently of its coefficient. For , the integral defining is holomorphic. With , multiplication by rotates the sector into , and multiplication by rotates into . Thus the two rotated transforms are holomorphic on their respective upper sectors.
Orient the contours as in the PDF: runs from infinity on the ray into zero and then out along the positive real axis; runs from negative real infinity into zero and then out along the ray. Both have their sector on their left. Smooth decay and integration by parts give in closed lower-half-plane sectors. The factor decays in the upper half-plane for . Close each sector by a large arc; the arc integral vanishes by Jordan lemma, including its short portion near the real axis. The Cauchy integral theorem therefore gives the rotated null contours for half-range Fourier inversion:Adding arbitrary constant multiples of these two zero integrals to ordinary Fourier inversion proves the asserted inversion formula. The constants are arbitrary in this part; selecting them later is what removes an unknown boundary trace.
Past exam of the mathematics course of the University of Cambridge 2006 iii Paper 86 1 b Solution Created 2026-10-03 Updated 2026-10-14
Define the initial Half-range Fourier transform , and, for each available boundary trace, its finite-time spectral boundary transformTemporarily let also denote the missing trace. Three integrations by parts in giveConsequently the backward-sign Airy half-line global relation isThe spatial transform is holomorphic below the real axis, while each finite-time is an entire function. Moreover, because .
Suppose the missing derivative has order , and put . Its contribution to the right-hand side is , where , , . Apply the inversion from the preceding part at time and selectThe rotated coefficients of that missing trace now equal minus its real-line coefficient. Its entire contribution is thereforeThe real-axis pieces cancel. What remains is the boundary of the middle upper sector, outward on and inward on . In this sector , andis bounded by . The factor decays exponentially throughout the closing arc, overcoming . There are no poles. Thus the Cauchy integral theorem proves the cubic-dispersion elimination of one missing boundary trace and removes every occurrence of the unknown .
For a compact explicit answer, use only the two prescribed traces to form . The three choices areFor each row the solution isAll quantities in this formula are transforms of the given data. On the contour rays is real, so the time exponential is oscillatory; the integrals use the usual limiting interpretation of Fourier inversion. The decay estimate used for elimination belongs to the middle sector, not to or , where can grow.
At , and the preceding inversion recovers . The spectral exponential satisfies the Airy equation with the required minus sign. Differentiating the finite-time amplitudes produces only derivatives of the Dirac delta supported at and zero rotated closed-contour contributions, so the interior equation also holds. Finally, two solutions with the same data have for their difference, so this representation gives zero: each of the three prescribed pairs determines the solution uniquely in the smooth decaying class.
Past exam of the mathematics course of the University of Cambridge 2006 iii Paper 86 2 b Solution Created 2026-10-03 Updated 2026-10-14
Let denote the Half-range Fourier transforms of , and let denote those of the upward derivatives . Also setIntegrate the tangential derivatives in the three spectral functions by parts. For example, , and . All corner values cancel in . The result is the semistrip Laplace spectral global relation
For , use the sine transformsReality of makes and real, so taking imaginary parts removes the unknown left-side normal derivative. At and the two consequences of the global relation areSubtracting these equations and then substituting back gives the semistrip Dirichlet-to-Neumann sine transforms entirely in terms of the prescribed Dirichlet boundary data:These are the requested transforms of itself. The bottom outward Neumann boundary data have the opposite sign. The apparent division at is handled by a continuous limit whenever the corresponding moments exist; there is no singularity for any .
Past exam of the mathematics course of the University of Cambridge 2006 iii Paper 86 3 a Solution 2026-10-14
Let , . Inverting the two orthogonal derivative systems gives, on the vertical axis,and, on the horizontal axis,Using the Wirtinger derivative , these become
Define the appropriate boundary transforms byThe first pair is holomorphic for ; the second pair consists of Half-range Fourier transforms, holomorphic for . Parametrizing the vertical boundary by gives , which must be retained. Substitution yields the quarter-plane oblique boundary spectral functions:Their signs follow from the stated clockwise boundary orientations: upward on the left and inward on the bottom.
Past exam of the mathematics course of the University of Cambridge 2007 iii Paper 86 1 b Solution Created 2026-10-03 Updated 2026-10-14
Set and , so . For boundary traces , defineThe Half-range Fourier transform of the equation is obtained by two integrations by parts:Solving this scalar equation gives the drift-diffusion half-line global relationIn particular the reflected relation is valid on , since there.
In the region between the real axis and , . Thus a boundary contribution admits an upward contour deformation from the real axis to . Large-contour estimates follow from the spatial exponential and the time integral; at the upper time endpoint one can integrate in time once or use a small contour displacement. The initial-data transform is retained on the real axis. Hence, if , ordinary inversion first givesFor the Dirichlet boundary condition, take . Subtract the null integral of the reflected time-dependent transform, using the inversion from part (a) with . The unknown derivative transform cancels because . This derives the Dirichlet spectral formula for half-line constant drift:Only initial and prescribed boundary data occur in this expression.
For the Neumann boundary condition, take . The reflected global relation reads . Solve for and substitute it in the preliminary representation. The leftover term is a null integral with multiplier , analytic above ; its pole at zero is below the contour. Thus the Neumann spectral formula for half-line constant drift isThere is no residue from the origin, since this elimination never moves the contour across it. The given derivative is the inward-coordinate derivative , not the outward derivative . The initial compatibility for this case is .
Past exam of the mathematics course of the University of Cambridge 2009 iii Paper 71 1 b Solution Created 2026-10-03 Updated 2026-10-14
Define the negative-exponential Half-range Fourier transformswhich are holomorphic for . Write and define the finite-time spectral boundary transformsIntegrate the local relation over , . The spatial boundary term at infinity vanishes by decay, and the term at is subtracted. Consequently the half-line linear dispersive Stokes global relation isFourier inversion on the real axis gives an initial-data integral plus an integral of . To put the boundary term on a complex contour, setFor , , so is the connected upper domain , . Orient with this domain on the left: from upper-left infinity down to , along the real segment to , and then to upper-right infinity.
The finite-time spectral boundary transforms are entire functions. In the upper regions outside , where , their time-integrated factors satisfy for . Together with , this permits contour deformation of the two remaining real-axis pieces to the curved boundary of . The resulting representation isThe contour orientation accounts for the plus sign in this convention. This formula still contains the two unknown derivative traces through .
Past exam of the mathematics course of the University of Cambridge 2009 iii Paper 71 3 Solution Created 2026-10-03 Updated 2026-10-14
Take the negative-exponential Half-range Fourier transform and setThe advection-diffusion equation has the local relation with flux . Integration over the half-line gives the half-line drift global relationFor the upper decay domainwrite . It is the region above , in particular above . Its boundary is oriented from upper-left infinity through to upper-right infinity, with the domain on the left. Fourier inversion and deformation of the boundary terms giveUse the dispersion symmetry elimination of a boundary trace . It preserves and maps into the lower half-plane. Because , the global relation at impliesThe last term contributes an holomorphic upper-domain integral multiplied by , so it vanishes upon closing the contour for . The solution representation with only known data is consequentlyFor the boundary value , direct integration givesThis quotient is an entire function of when its apparent singularities at are filled by their limits. Those points are not genuine forcing poles of the finite-time transform.
To obtain an exponentially decaying spectral integrand, choose and the exponential-decay contour for half-line drift diffusionDeform to . No pole is crossed: the initial-data denominator in that boundary integral has its only pole at , which lies below since . The apparent singularities of the forcing transform are removable. In the swept outer sectors, has the appropriate bounded growth for the deformation. The contour formula becomesEvaluate the second quotient as a removable expression at , rather than splitting it into artificial residue terms. On either ray,Since , the transient factors have Gaussian decay as . The nontransient forcing term is and thus also decays exponentially for every . The real-axis integral has the Gaussian factor . These estimates provide the requested improvement over integration along .
Upper cubic-dispersion contour and exponentially decaying drift-diffusion contour, with their orientations
. Details. The first panel shows the cubic domain from Question 1. The second uses and ; its marked initial-data pole corresponds to and lies below both boundary contours.
An independent real-kernel form also makes the initial and boundary traces explicit. Apply the Dirichlet gauge transform for constant drift, , and then multiply by to obtain the heat equation. The odd-reflected heat kernel for initial data and its Dirichlet boundary-forcing heat-kernel formula yieldThe first kernel tends to the initial delta kernel on as and vanishes at . For the second kernel, the substitution gives the unit-mass approximate boundary delta as , so its trace is ; it vanishes initially for fixed . Differentiating the kernels for verifies the advection-diffusion equation. The integrals converge for every positive , even when the exponentially weighted initial datum grows, because the spatial Gaussian controls that growth. Thus this gives the same decaying solution without introducing an additional restriction on .
For a general decaying initial datum, an unweighted Fourier sine transform does not directly diagonalize the drift operator. DefineTwo integrations by parts for and one for giveThe cosine transform remains unknown, so this is not a closed sine-transform evolution. In contrast, the weighted sine transform for half-line drift diffusion of is closed:When the weighted initial transform exists, Fourier sine inversion gives . This method requires suitable decay of , not merely decay of . For the exponential datum it is an ordinary integrable sine transform only when . At one would need a generalized or regularized transform instead; the contour and real-kernel formulas above already work without that restriction. Therefore the ordinary sine transform of is not a closed solution method; a weighted sine transform works under the stated extra weighted-decay condition.
Past exam of the mathematics course of the University of Cambridge 2010 iii Paper 70 1 a Solution Created 2026-10-03 Updated 2026-10-14
Use a Fourier transform parallel to the boundary. Splitting its traces into right- and left-supported parts gives Half-range Fourier transforms and , analytic respectively above and below a common inversion contour. A small positive imaginary part of the wavenumber implements the limiting absorption principle and separates the incident poles and outgoing branch points. Solve the transformed differential equation normal to the boundary using its outgoing or decaying solution. The boundary conditions then yield a Wiener-Hopf equation of the formFactor its Wiener-Hopf kernel as , with each factor analytic and nonzero in its designated half-plane. Divide by and split , allocating poles according to the incident-wave prescription. ThenThe two sides continue to a common entire function. Their growth at infinity, inherited from the field's edge behavior, determines that function, usually a constant or a polynomial; in a decaying case it is zero. Solve for the unknown transforms and apply Fourier inversion, preserving the outgoing contour prescription.
The principal analytic results used are as follows. The Paley–Wiener theorem and its half-line Laplace-transform version relate support on a half-line to holomorphy in a half-plane, with growth or square-integrability bounds. The Cauchy integral formula and Sokhotski–Plemelj theorem provide additive splitting: a Cauchy integral of a sufficiently decaying jump has upper and lower boundary values with that prescribed difference. Applying the same construction to a continuous logarithm of a nonvanishing scalar Wiener-Hopf kernel gives Wiener-Hopf factorization when its winding number is zero; a nonzero index requires an explicit index factor. The identity theorem gives analytic continuation across the common strip. Finally Liouville's theorem makes a bounded entire function constant; its polynomial-growth extension bounds the possible degree. The physical edge and radiation conditions select the remaining constants. Zeros, branch cuts, nonzero index and insufficient decay must be accounted for rather than discarded during splitting.
Past exam of the mathematics course of the University of Cambridge 2012 iii Paper 78 2 Solution Created 2026-10-03 Updated 2026-10-14
Suppress the common time factor and use the Fourier transform conventionA right Half-range Fourier transform is analytic above its convergence line and a left transform below it. For the limiting absorption principle with this time convention take , , , before taking . SetThis is the outgoing acoustic square-root branch: at a propagating real wavenumber, . Put and . Across the fluid part of , the field and its normal derivative are continuous; on the sheet both sides have the same normal velocity. The outgoing Helmholtz equation solutions therefore have equal normal derivatives and opposite scattered traces:The jump is supported on , and so is a minus transform.
The linear fluid equation and the sheet velocity imply on either face. The incident contribution to the left derivative transform is . Writing , it follows thatThe upward net pressure is lower minus upper, hence in transform space. If , the pinned endpoint givesCombining these identities gives the Wiener-Hopf equationThis is the plane-wave forcing of a pinned elastic half-sheet.
Let and assume initially that the distinguished points are distinct. Besides the branch points , has simple poles at . Its physical-sheet zeros solve the fluid-loaded dispersion relationFor real positive frequency there is exactly one positive real root : the left side increases strictly from zero to infinity on that interval. Equivalently, with , . Its other roots have negative real part and do not belong to this outgoing sheet. Continue with small absorption; lie below the real line and their negative partners above it. The Wiener-Hopf factorization assigns the lower branch cut and pole to , and the upper branch cut and pole to . The continued has a zero at , and at ; these are poles of their reciprocals, rather than poles of the factors. Branch cuts can be drawn away from the real line into the corresponding half-planes.
For this standard assignment a common strip of analyticity and nonvanishing isThe strip shrinks to the real contour as absorption is removed. The factors continue meromorphically beyond their designated half-planes; the allocation of the poles and branch points is part of the radiation condition. The incident pole belongs above the inversion contour. For incidence with the real contour is a direct choice. Other nongrazing angles are obtained by analytic continuation with the incident pole kept on its prescribed side, deforming the contour locally if necessary. Coincident distinguished points and grazing incidence are treated by the corresponding limits, not by dividing by a coincident pole.
Divide the Wiener-Hopf equation by and use pole subtraction in a Wiener-Hopf equation. With , the minus part of isIndeed these are exactly the incident-pole and upper bare-sheet-pole residues. At the lower bare-sheet pole , the forcing pole is canceled by the pole of before splitting. Thus is analytic on the plus side of the contour. The separated equation isWith the stipulated ,The scattered field is consequentlyThe full time-dependent density perturbation is the incident field plus . The two traces at follow by limiting from above and below. A constant rescaling of the two factors does not change this field.
To determine the endpoint slope, reconstruct the sheet transform using the fluid condition:At the continued has residue . Therefore the derivative transform generically has the lower-plane poleThis pole produces a forbidden incoming bare-sheet wave in the reconstructed displacement: travels towards the endpoint from . A minus transform of the specified outgoing solution must be analytic there. The incoming-pole cancellation at a pinned membrane edge is preciselyFor generic parameters this determinesThe lower pole is removed; the upper zero of can still produce the legitimate outgoing evanescent acoustic surface wave, whose phase travels to negative . This distinction separates the spurious bare-sheet wave from the coupled fluid-loaded mode. No explicit factorization has been used.
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 69 1 i Solution Created 2026-10-03 Updated 2026-10-06
Use the spectral parameter for a linear boundary value problem and define the dispersion relation . Direct differentiation gives the divergence formIndeed the coefficient of left over after expansion is , and the remaining factor is . Thus this is equivalent to the advection-diffusion equation for every .
Introduce the Half-range Fourier transforms and finite-time spectral boundary transformswhere is the unknown normal derivative with the positive- convention. The outward normal at zero instead gives . The spatial transforms are analytic for and continuous on the real axis under the stated decay assumptions. Integrating the divergence form on gives the global relationThe sign follows from the lower spatial endpoint: the integrated spatial derivative is minus its value at zero. This sign will determine the boundary-forcing term in the solution.


