Use the radial reduction of the three-dimensional wave equation and extend oddly in . Write , where is the homogeneous wave equation solution with the prescribed Cauchy data, and has zero Cauchy data. With and , the D'Alembert formula gives
Both odd initial profiles have compact support, so
The Duhamel principle, applied to , gives
Now write with . The lower integration limit is , so this domain of dependence never crosses the axis. Intersecting its integration interval with the support of the source leaves a subset of , of length at most one. On this interval,
The outgoing shell source estimate for a radial wave therefore yields
Finally , and thus
This constant depends only on the Cauchy data and the fixed unit bound for the source. The logarithm comes from integrating the shell's accumulated forcing, whereas the factor comes from division by .
We establish a quantitative almost global existence for wave equations estimate. Take , fix an integer , and use the commutation vector fields for the wave equation from the preceding part. Put and define the commuted wave energy
All these L2 norms are finite on any smooth existence interval by finite propagation speed. At , the polynomial coefficients of the vector fields are bounded on the fixed compact support of the Cauchy data. Whenever a higher time derivative occurs, use and its differentiated versions to express it in terms of initial spatial derivatives. Every term contains at least one factor of ; consequently
for a constant depending only on finitely many derivatives and the support radius of .
The commutators are constant linear combinations of translations. Together with and the Leibniz rule, this shows that each commuted source is a finite linear combination of products
This statement includes the extra copies of the original source produced by the scaling vector field. In each product put the factor with fewer commutations in the Lp norm and the other in the L2 norm. The lower order is at most . Applying the Klainerman-Sobolev inequality to costs at most two additional commutations; commuting those past introduces only lower-order translations. Since ,
The inhomogeneous wave energy estimate now gives
Let . Use a bootstrap argument with up to the smaller of and the maximal existence time. The energy estimate improves this to
For each fixed ,
Choose so that for every . Then , a strict improvement. A continuity argument closes the bootstrap argument.
Finally, the translation terms in control ordinary spatial Sobolev norms of . The missing L2 norm of satisfies
Thus the full local-existence Sobolev norms remain bounded on this finite interval. The smooth continuation criterion for semilinear wave equations extends the solution past any finite endpoint before . To see smooth persistence explicitly, the tame Sobolev product estimate gives . Ordinary differentiated wave energy estimates therefore bound each higher derivative energy by its initial value times . This is finite on the interval already controlled by the base commuted wave energy; no separate is needed for each derivative order. Therefore
For the zero solution is global. The same energy estimate in fact permits an exponential lower bound for the lifespan, which is stronger than any fixed inverse power.
The sign convention makes this a defocusing semilinear wave equation:
Its wave energy includes a nonnegative potential term:
For a smooth function solution, finite propagation speed preserves compact support on finite time intervals. Differentiate under the integral and use integration by parts:
Equivalently the local conservation law has density and flux . All three terms are nonnegative, and forces both Cauchy data to vanish. Hence this is a positive conserved energy, rather than the indefinite energy associated with the opposite sign.
The opposite sign is the focusing semilinear wave equation . Begin with a spatially constant solution, reducing the partial differential equation to the ordinary differential equation . Substitution of gives
For a nonzero profile, equality of powers and coefficients gives and . Choose
To obtain compact support, take a smooth cutoff function equal to one on and zero outside , and prescribe
These are smooth, compactly supported Cauchy data. By finite propagation speed, the local solution agrees with throughout for , where is its maximal forward smooth existence time.
For completeness, the semilinear domain of dependence assertion follows by comparing two solutions: their difference obeys , with . On any compact time interval before on which the solutions are smooth, is bounded in the backward light cone. Add to the shrinking-ball wave energy; its derivative is bounded above by times that energy, with the same nonpositive boundary flux. Zero initial difference and the Gronwall inequality give there.
If , the identity at the origin would imply as , contradicting smoothness at . Thus
If the solution loses regularity earlier, that is already finite-time blowup. The usual smooth continuation criterion for semilinear wave equations precludes a finite maximal time with all continuation norms bounded. This localized ordinary differential equation blowup for a wave equation therefore supplies the required compactly supported examples.
Compatible Cauchy data for a wave map are and : thus and . Smooth localized wave map Cauchy data equal a constant with zero velocity outside a compact set. It is , rather than the sphere-valued map itself, that has compact support. The geometric constraints propagate under the wave map equation.
Small data global regularity for wave maps holds in four spatial dimensions. Smallness is measured in sufficiently high weighted Sobolev norms relative to a constant map, with localized compatible Cauchy data. The vector field method for wave equations gives derivative decay . This is time-integrable, so commuted wave energy estimates close a small-data bootstrap argument for the derivative-quadratic semilinear wave equation. Higher regularity persists. No smallness of energy alone is asserted.
One prescribes analytic Cauchy data: the value of and one first derivative transverse to , for example
where and are real analytic on . Being a non-characteristic hypersurface allows the equation to solve for the second derivative in the transverse direction. The Cauchy-Kovalevskaya theorem then gives one and only one local real analytic solution near .
Assume and set
The travel-time coordinate for a one-dimensional variable-speed wave equation
sends the initial interval to . By the characteristic curves for speed one minus y squared, the two characteristic coordinates are and . The finite propagation speed and uniqueness theorem for hyperbolic partial differential equations therefore give the maximal characteristic diamond
Equivalently,
In the plane this is a diamond with vertices and ; transforming back bends its four sides into the characteristic curves found in part 3(c). Beyond any one of those sides, a point's backward characteristics meet outside , where no Cauchy data were prescribed, so uniqueness cannot be extended farther.
The initial line has conormal , and the principal symbol on this conormal is . It is therefore a non-characteristic hypersurface at every . The equation's coefficients and the prescribed Cauchy data and are real analytic functions. The Cauchy-Kovalevskaya theorem consequently gives a unique analytic solution in a neighbourhood of for every
The initial line is , whose conormal is . Evaluating the principal symbol on it gives
It is therefore a non-characteristic hypersurface at exactly when . At such a point the equation can be written
whose right-hand side is real analytic locally, and the prescribed Cauchy data are also real analytic. The Cauchy-Kovalevskaya theorem consequently gives a unique local analytic solution exactly at the points
Put
The assumed energy estimate for the linear wave equation and the first nonlinear estimate give, for ,
Choose and then choose so small that . Then maps the closed ball into itself.
For , the difference solves the linear equation with zero Cauchy data and forcing . The second nonlinear estimate therefore gives
Shrinking once more makes the coefficient strictly smaller than one. Since is a Banach space and its closed ball is complete, is a contraction on .
The scalar Cauchy-Kovalevskaya theorem says that a partial differential equation solved for its highest derivative normal to a real-analytic non-characteristic hypersurface, with real-analytic coefficients and Cauchy data, has a unique local real-analytic solution. In coordinates, an equation
has such a solution near the origin when and the prescribed values of for are real analytic.
Choose a real-analytic primitive of near zero and apply the theorem to the scalar Laplace equation
The line is non-characteristic because the coefficient of is one. Define
Then and , while equality of mixed derivatives and the Laplace equation give
Thus is the required local real-analytic solution.
Write
Differentiating the prescribed identity in its two tangential directions gives
The unit normal is , so the second item of Cauchy data becomes
Consequently
Substitution into the principal symbol from part a shows that the graph is non-characteristic exactly where
The Cauchy-Kovalevskaya theorem says that an order- scalar quasilinear partial differential equation with real-analytic coefficients has a unique local real-analytic solution near each point of a real-analytic non-characteristic hypersurface, provided the prescribed Cauchy data
are real analytic there. The uniqueness is among local real-analytic solutions agreeing with all of those data.
Shrinking cone energy argument Created 2026-10-06 Updated 2026-10-14
For the homogeneous speed-one wave equation, integrate its wave energy density over . The moving boundary contributes , while the usual flux contributes . Their sum is . Zero Cauchy data in the initial ball therefore force zero solution in its backward light cone.
For whole-line Cauchy data with support contained in , the displayed inclusion holds at . A short check uses D'Alembert's formula: if , both sampled endpoints and the whole interval of integration lie to the right of , so all contributions vanish; the argument for is identical. The inclusion can be strict, and a nonzero response at the first permitted arrival is not guaranteed.