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Beltrami equation

Partial differential equation

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  • 9 chapters

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Through Mathematics and Complex plane

∂w∂z¯=μ∂w∂z.

for w a complex distribution of the complex variable z in some open set U, with derivatives that are locally L2, and where μ is a given complex function in L∞(U) of norm less than 1, called the Beltrami coefficient, and where ∂/∂z and ∂/∂z¯ are Wirtinger derivatives. Classically this differential equation was used by Gauss to prove the existence locally of isothermal coordinates on a surface with analytic Riemannian metric. Various techniques have been developed for solving the equation. The most powerful, developed in the 1950s, provides global solutions of the equation on C and relies on the Lp theory of the Beurling transform, a singular integral operator defined on Lp(C) for all 1 < p < ∞. The same method applies equally well on the unit disk and upper half plane and plays a fundamental role in Teichmüller theory and the theory of quasiconformal mappings. Various uniformization theorems can be proved using the equation, including the measurable Riemann mapping theorem and the simultaneous uniformization theorem. The existence of conformal weldings can also be derived using the Beltrami equation. One of the simplest applications is to the Riemann mapping theorem for simply connected bounded open domains in the complex plane. When the domain has smooth boundary, elliptic regularity for the equation can be used to show that the uniformizing map from the unit disk to the domain extends to a C∞ function from the closed disk to the closure of the domain.

Metrics on planar domains

Consider a 2-dimensional Riemannian manifold, say with an (x, y) coordinate system on it. The curves of constant x on that surface typically don't intersect the curves of constant y orthogonally. A new coordinate system (u, v) is called isothermal when the curves of constant u do intersect the curves of constant v orthogonally and, in addition, the parameter spacing is the same — that is, for small enough h, the little region with a≤u≤a+h and b≤v≤b+h is nearly square, not just nearly rectangular. The Beltrami equation is the equation that has to be solved in order to construct isothermal coordinate systems.

To see how this works, let S be an open set in C and let

ds2=Edx2+2Fdxdy+Gdy2

be a smooth metric g on S. The first fundamental form of g

g(x,y)=(EFFG)

is a positive real matrix (E > 0, G > 0, EG − F2 > 0) that varies smoothly with x and y.

The Beltrami coefficient of the metric g is defined to be

μ(x,y)=E−G+2iFE+G+2EG−F2

This coefficient has modulus strictly less than one since the identity

(E−G+2iF)(E−G−2iF)=(E+G+2EG−F2)(E+G−2EG−F2)

implies that

|μ|2=E+G−2EG−F2E+G+2EG−F2<1.

Let f(x,y) =(u(x,y),v(x,y)) be a smooth diffeomorphism of S onto another open set T in C. The map f preserves orientation just when its Jacobian is positive:

uxvy−vxuy>0.

And using f to pull back to S the standard Euclidean metric ds2 = du2 + dv2 on T induces a metric on S given by

ds2=du2+dv2=(ux2+vx2)dx2+2(uxuy+vxvy)dxdy+(uy2+vy2)dy2,

a metric whose first fundamental form is

(ux2+vx2uxuy+vxvyuxuy+vxvyuy2+vy2).

When f both preserves orientation and induces a metric that differs from the original metric g only by a positive, smoothly varying scale factor r(x, y), the new coordinates u and v defined on S by f are called isothermal coordinates.

To determine when this happens, we reinterpret f as a complex-valued function of a complex variable f(x+iy) = u(x+iy) + iv(x+iy) so that we can apply the Wirtinger derivatives:

∂z=12(∂x−i∂y),∂z¯=12(∂x+i∂y);dz=dx+idy,dz¯=dx−idy.

Since

fz=((ux+vy)+i(vx−uy))/2
fz¯=((ux−vy)+i(vx+uy))/2,

the metric induced by f is given by

ds2=|fzdz+fz¯dz¯|2=|fz|2|dz+fz¯fzdz¯|2.

The Beltrami quotient of this induced metric is defined to be fz¯/fz.

The Beltrami quotient fz¯/fz of f equals the Beltrami coefficient μ(z) of the original metric g just when

((ux+vy)+i(vx−uy))(E−G+2iF)
=((ux−vy)+i(vx+uy))(E+G+2EG−F2).

The real and imaginary parts of this identity linearly relate ux, uy, vx, and vy, and solving for uy and vy gives

uy=Fux−EG−F2vxEandvy=EG−F2ux+FvxE.

It follows that the metric induced by f is then r(x, y) g(x,y), where r=(ux2+vx2)/E, which is positive, while the Jacobian of f is then rEG−F2, which is also positive. So, when fz¯/fz=μ(z), the new coordinate system given by f is isothermal.

Conversely, consider a diffeomorphism f that does give us isothermal coordinates. We then have

μ(z)=(ux2+vx2)−(uy+vy)2+2i(uxuy+vxvy)(ux2+vx2)+(uy2+vy)2+2(ux2+vx2)(uy2+vy2)−(uxuy+vxvy)2,

where the scale factor r(x, y) has dropped out and the expression inside the square root is the perfect square ux2vy2−2uxvxuyvy+vx2uy2. Since f must preserve orientation to give isothermal coordinates, the Jacobian uxvy−vxuy is the positive square root; so we have

μ(z)=((ux+iuy)+i(vx+ivy))((ux+iuy)−i(vx+ivy))((ux+vy)+i(vx−uy))((ux+vy)−i(vx−uy)).

The right-hand factors in the numerator and denominator are equal and, since the Jacobian is positive, their common value can't be zero; so μ(z)=fz¯/fz.

Thus, the local coordinate system given by a diffeomorphism f is isothermal just when f solves the Beltrami equation for μ(z).

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