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Course 4Book 4A: Function Spaces and Sobolev SpacesChapter 11
Hölder Spaces
Measuring roughness, and why Hölder spaces are the right setting for regularity.
Read with Evans, Partial Differential Equations, §5.1 (Hölder spaces), which is short; Gilbarg and Trudinger, Elliptic Partial Differential Equations of Second Order, chapter 4, is the reference for Hölder estimates when Book 6A needs them.
Continuity says a function changes little over small distances. Hölder continuity says how little: for some exponent . The exponent measures roughness on a continuous scale between merely continuous ( near ) and Lipschitz (), and the corresponding spaces sit between and . Morrey's inequality (4A.10 Sobolev Embeddings and Critical Exponents) already showed that Sobolev functions with enough integrability are Hölder continuous.
The reason for a whole chapter is a fact about elliptic and parabolic equations. If is continuous, need not be twice differentiable: the classical spaces don't fit the Laplacian. But if is Hölder continuous, then is twice differentiable with Hölder second derivatives (Schauder's estimates, 6A.6 Parabolic Regularity). Hölder spaces are the spaces in which the Laplacian, and the heat operator, gain exactly two derivatives. That is why the existence theory for nonlinear parabolic equations, and in particular the short-time existence of Ricci flow, is set in Hölder spaces (6A.7 Nonlinear Parabolic Equations, 11A.3 Short-Time Existence and Uniqueness). This short chapter defines them, proves their compactness properties, and explains with an explicit example why would not do.
By the end of this chapter you will be able to:
- compute Hölder seminorms and decide which a given function belongs to;
- prove that Hölder spaces are complete and that is compact for on compact sets;
- give a function with continuous Laplacian that is not , and state Schauder's estimate that rules this out in Hölder spaces;
- relate Hölder exponents to the roughness of real signals and random paths.
How rough is a random path?
The path of a particle in Brownian motion, the jittering of pollen grains in water that Robert Brown observed in 1827, is modelled mathematically by a random continuous function whose increments are independent, with mean and variance . Its typical displacement over a time is therefore about , much larger than for small , so the path can't be differentiable. Norbert Wiener constructed this process rigorously in 1923, and it is now known that, with probability , the path is Hölder continuous with every exponent , and with no exponent , and that it is differentiable at no point (Paley, Wiener and Zygmund, 1933). The exponent is the roughness of Brownian motion: zooming in by a factor in time and in space gives a path with the same statistics (Figure 11.1).
Natural records are rougher or smoother than this. The hydrologist Harold Edwin Hurst, studying centuries of records of the Nile's floods to size the reservoirs planned at Aswan, found in 1951 that the range of cumulative departures from the mean grew like with over time spans , not like as independent random fluctuations would give: wet and dry years clustered. Benoit Mandelbrot and John van Ness introduced fractional Brownian motion in 1968 as a model with this scaling: its paths are Hölder continuous with every exponent below its Hurst exponent . Estimating Hölder or Hurst exponents of measured signals (river flows, financial prices, rough surfaces) is now a standard way of quantifying how rough they are, though the estimates need care.
Hölder spaces
Let and . The Hölder seminorm of is
is the space of bounded continuous with , normed by . For an integer , consists of functions whose derivatives up to order are bounded and whose -th derivatives are in , with
For the seminorm is the Lipschitz constant. For only constants qualify (on a connected set the difference quotient would tend to , forcing the derivative to vanish), which is why . The standard example is a power of the distance.
On , with has : by the concavity of , , with equality when . It is not in for any , since as (Figure 11.2). So the exponent of a power singularity is exactly its Hölder exponent.
is a Banach space.
Proof. For : a Cauchy sequence converges uniformly to some (2B.5 Uniform Convergence and Arzelà–Ascoli). For fixed , for ; letting gives . For , apply this to the derivatives, using 2B.5 Uniform Convergence and Arzelà–Ascoli's theorem on uniform limits of derivatives.
Hölder spaces have one awkward feature: smooth functions are not dense in them. The function can't be approximated in norm by smooth functions, because near any smooth function has , while for the ratio is . (The closure of the smooth functions is the "little Hölder space".) Hölder spaces are also not separable. Neither fact matters for the existence theory, which uses completeness and the compactness below.
Compactness
Let be compact and . Then bounded sets in are precompact in . Likewise is compact.
Proof. A bounded set in is uniformly bounded and equicontinuous ( for all its members), so by Arzelà–Ascoli (2B.5 Uniform Convergence and Arzelà–Ascoli) every sequence has a uniformly convergent subsequence. To upgrade to convergence, use the interpolation inequality
which follows from . Applied to , whose -seminorm is bounded and whose sup tends to , it shows is Cauchy in .
The pattern is the one of the whole book: a stronger norm bounded, a weaker norm convergent, and an interpolation inequality between them (3A.7 Lᵖ Spaces and Jensen’s Inequality). It is how limits are taken in the existence theory for nonlinear PDE, and in the compactness theorems for Ricci flows, where bounds on curvature in a Hölder norm give convergence in a slightly weaker one (11B.3 Compactness of Ricci Flows).
Why Hölder and not
For the Laplacian in the plane, data do not give solutions.
On the disc in , let
with . A computation (Exercise 11.10) gives, for ,
which tends to as : so extends continuously to the whole disc. But as . So is a solution of with continuous, and .
The failure is a slow, logarithmic one, and it disappears as soon as the data are a little better than continuous.
Let . If in a ball and , then and
with depending only on and . The same holds for uniformly elliptic operators with Hölder continuous coefficients, and for the heat equation in parabolic Hölder spaces.
The proof, by comparison with the fundamental solution (4A.8 Distributions and Weak Derivatives) and careful estimates of singular integrals, or by approximation with harmonic functions, is in 6A.6 Parabolic Regularity (Gilbarg–Trudinger, chapter 4). The point here is the form: the operator gains exactly two derivatives, measured in the same Hölder exponent. That makes the Laplacian an isomorphism between suitable and spaces, which is what the perturbation and contraction arguments of 4A.1 Banach Spaces and Bounded Operators and 2B.9 The Inverse and Implicit Function Theorems need. In it is not an isomorphism (by the example), and neither is it from to for any . Hölder spaces are the classical spaces in which elliptic and parabolic equations are well posed.
In linear elastic fracture mechanics, the displacement of the material near the tip of a crack behaves like times a function of angle, where is the distance to the tip, so the stresses (derivatives of the displacement) grow like . The displacement is Hölder continuous with exponent at the tip and no better. M. L. Williams (1957) derived this behaviour from the equations of elasticity, and George Irwin (1957) built fracture mechanics around the coefficient of the singularity, the stress intensity factor: a crack grows when that coefficient reaches a critical value characteristic of the material. Engineers designing against fracture thus work directly with a Hölder- singularity, a reminder that the regularity theory of elliptic equations has corners (literally) where it stops: at boundary points that are not smooth, solutions are only Hölder continuous, with an exponent set by the angle.
Schauder theory, interior and up to the boundary, for elliptic and parabolic equations (6A.6 Parabolic Regularity); short-time existence for quasilinear parabolic equations by contraction in parabolic Hölder spaces (6A.7 Nonlinear Parabolic Equations); and the short-time existence of Ricci flow, where after DeTurck's modification the flow is a strictly parabolic system for the metric, solved in exactly these spaces (11A.3 Short-Time Existence and Uniqueness). In compactness theorems, bounds on metrics in harmonic coordinates give convergence for , which is the form in which Cheeger–Gromov convergence is often stated (9B.4 Convergence of Manifolds).
History
Rudolf Lipschitz introduced his condition in 1864 (in work on Fourier series) and used it for differential equations in 1876; Otto Hölder used the fractional version in his 1882 dissertation on potential theory. Juliusz Schauder proved his estimates in 1934, building on work of Hölder, Korn and Lichtenstein. Robert Brown described the motion of pollen particles in 1827, Albert Einstein explained it in 1905, and Wiener constructed the mathematical process in 1923; Paley, Wiener and Zygmund proved nowhere differentiability in 1933. Hurst's Nile study appeared in 1951 and Mandelbrot and van Ness's fractional Brownian motion in 1968.
Banach spaces carry analysis into infinite dimensions, where the unit ball is not compact (Riesz). Completeness alone gives uniform boundedness, open mapping and closed graph (Baire). Hahn–Banach supplies enough functionals, and identifies duals: for , measures for . Hilbert spaces add projections, Riesz representation and orthonormal bases, and Lax–Milgram gives weak solutions. The Fourier transform diagonalises derivatives and is an isometry of . Weak convergence restores compactness in reflexive spaces, and with convexity the direct method gives minimisers. Compact self-adjoint operators have eigenbases, and the Laplacian on a bounded domain has a discrete spectrum. Distributions differentiate everything; Sobolev spaces are the functions with weak derivatives in , with Poincaré, Sobolev and Morrey inequalities, compact embeddings below the critical exponent, and concentration at it. Hölder spaces are where elliptic equations gain exactly two derivatives.
Everything needed to state and solve linear PDE is now in place: spaces (, , ), compactness (Rellich, Arzelà–Ascoli), existence (Lax–Milgram, the direct method) and spectra. Book 5A is optional: it revisits harmonic functions and conformal geometry from the complex-analytic side, ending at Ricci flow on surfaces. Book 6A, starting with 6A.1 What a PDE Is, is the main line: the heat equation, in full.
Exercises
Find the best Hölder exponent on of (a) ; (b) (with value at ); (c) on ; (d) , as an element of .
Solution
(a) . (b) Every , not (the derivative is unbounded). (c) Continuous but no positive exponent: . (d) , so .
Show that , so is closed under products, and that if is Lipschitz then . Show also that composing two Hölder functions with exponents and gives exponent .
Prove for , and use it to show that is compact. Why is the embedding (the identity) not compact? (Use -type bumps, or 4A.1 Banach Spaces and Bounded Operators.)
For with (a harmonic polynomial of degree ) and radial, show in the plane. With , compute and , and deduce the formula for in Example 11.5. Then show is unbounded near .
Solution
, using for a homogeneous polynomial of degree . So . With the given : , and . On the -axis, and ; the last two terms are bounded and .
If is a Brownian motion, show (assuming the definition) that has independent increments with variance , so it is again a Brownian motion. Explain why this self-similarity is consistent with Hölder exponent exactly and with no larger one.
Let on and set , on , so . Using the Schauder estimate on for and translating back, show
Every term has the same "units" (those of ): this is the scale-invariant form of the estimate. In 11B.4 Singularities and 12B.3 The Canonical Neighbourhood Theorem, estimates for Ricci flow are always used in scale-invariant form, so that they survive the rescalings at singularities; checking the powers of as here is how one confirms an estimate is stated correctly.
Solution
and ; similarly and . Substituting into the estimate for and dividing by gives the stated form.
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