For a surface of revolution whose induced metric is , with and smooth on a coordinate interval, define . Then and the conformal factor gives . This proves the rescaled metric is locally the Euclidean metric without solving a curvature equation. Poles and places where is not a coordinate must be treated in other charts; the angular coordinate is also understood locally.
Elliptic paraboloid 2026-10-07
An elliptic paraboloid is a smooth bowl-shaped quadratic surface with elliptical horizontal sections. In the circular case , it is a surface of revolution. For , polar coordinates give the parametrization and upward vector area element . A band between two positive heights has two boundary circles and no cap.
The surface of revolution
is geodesically incomplete: a meridian reaches the missing origin in finite length. Its Gaussian curvature, computed using the curvatures of a parametrized surface of revolution, is
which tends to infinity as . Every finite-time endpoint of a constant-speed geodesic must approach the origin, the only finite point in the ambient closure missing from , so this surface satisfies the curvature-blowup criterion.
For , rotate the unit-speed profile
near . Since , the resulting regular surface of revolution has . At its principal curvatures are and , so the point is not umbilical when and no neighbourhood of it lies on a sphere.
Parametrize the surface of revolution by . The coordinate tangent vectors have squared lengths and , and inner product zero. Thus the first fundamental form of an arc-length surface of revolution is .
For an arc-length parameter , the geodesic equations are
These follow either from the metric's Christoffel symbols or from the Euler-Lagrange equation for . On a parallel , unit speed requires ; the first geodesic equation then holds exactly when . Thus geodesic parallels of a surface of revolution are precisely the critical points of the radius function.
To obtain any prescribed positive integer , set
The function is bounded and integrable. Choose so , and choose . Then , is smooth, and . The derivative vanishes at exactly . Also , so different meridian parameters give different heights. The resulting surface has exactly geodesic parallels.
For explicit sketches, use the following two radius functions, again with :
Here has only the zero , while has exactly the zeros . Both radii stay positive and both derivatives have absolute value below one. The highlighted rings are the geodesic parallels; the surfaces continue beyond the displayed window.
Figure 1.
Surfaces of revolution with exactly one and exactly two geodesic parallels
.
If every parallel is a geodesic, then everywhere, so is a positive constant. The arc-length condition gives ; smoothness forces a constant sign, hence . The surface is a circular cylinder of radius . It is a circular cylinder because the meridian is a straight line parallel to the axis.
Along a sufficiently smooth stationary curve, differentiation and the Euler-Lagrange equation give the Beltrami identity:
The cancellation uses the absence of explicit dependence.
For an axisymmetric surface of revolution, its area is . A smooth positive-radius minimizer is stationary, so the Beltrami identity, with the constant factor omitted, gives
Equivalently the Euler-Lagrange equation gives , whence . The first integral selects
Equal radii at imply (subtract the two cosh values), giving
This is a catenoid. The conclusion is a necessary form for a smooth connected minimizer; it does not declare every stationary catenoid a minimum.
Put . The boundary equation is . Its derivative is , so its unique critical point solves . The left side increases strictly from zero to infinity. Thus decreases to a unique minimum and then increases, diverging as and . There are exactly two positive values of when
At equality there is one value, and below it there is none.
To match the printed second variation convention, write ; its is the quadratic coefficient, half the second derivative with respect to . Expanding the area integrand gives
On the catenoid these coefficients are and . Integrate the mixed term by parts; the boundary term is zero because . Since , this yields
This is the axisymmetric second variation of a catenoid, with the explicitly stated quadratic-coefficient convention.
Stokes theorem equates the circulation around the induced boundary orientation of an oriented surface to the normal flux of curl:
The usual version requires a piecewise smooth oriented surface and a vector field continuously differentiable on a neighbourhood of it. We use the upward orientation wherever the surface is a graph; each outer circle is counterclockwise viewed from above, and an inner circle is clockwise.
Write . The surface of revolution has with . For , it is a disk-shaped cap of a two-sheeted hyperboloid, running from to . For , it is a right circular cone, , including its apex. For , it is an annular strip of a one-sheet hyperboloid, between the circles and .
Figure 1.
Disk cap, cone and annular hyperboloid strip in the three positive-parameter regimes of Stokes' theorem
.
For , differentiation of the graph gives and , so the upward vector surface element of a graph and its scalar area are
For this graph expression is singular at the lower circle because the surface has a vertical tangent there, rather than a singular geometric surface. A regular parametrization is
It proves that the graph surface integral is interpreted by its integrable endpoint limit. The same parametrization works away from the pole or apex in the other regimes.
Direct differentiation of the first vector field gives
Its surface integral is twice the projected area, namely for and for . On an oriented circle of radius , . The outer circulation is ; an inner circle, when present, contributes . Thus
At , excise a small apex circle of radius , apply Stokes theorem to the smooth truncated cone, and let . The removed flux and its inner circulation are both , so the limiting equality holds. This avoids silently applying a smooth-surface theorem at the cone's nonsmooth apex.
The second vector field is the azimuthal inverse-radius vector field, . Away from the axis,
The other two curl components vanish because the field is independent of and has zero component. On any positively oriented circle around the axis, , so its circulation is , independent of radius. Therefore
For the surface avoids the axis, so Stokes theorem applies directly and returns zero curl flux. For the disk cap meets the axis, and for the apex lies on it: is undefined there, so the neighbourhood hypothesis of Stokes theorem fails. Removing a small circle gives cancelling inner and outer circulations; the inner circulation remains as its radius tends to zero. Hence it cannot be discarded as it could for . A nonzero circulation here is compatible with zero curl away from the excluded axis.
Constant Gaussian curvature one gives , so, after a shift of the arc-length parameter, with on an interval contained in . To close the surface by adding only two points, the limiting parallels at both ends must collapse to points on the axis. If an end had limiting radius , it would contribute a whole missing circle, which two added points cannot supply. Thus the parameter interval is the full interval between consecutive zeros, and its two ends are .
At a smooth axis point the tangent plane of a surface of revolution is invariant under all rotations about the axis, so it must be horizontal. The unit meridian tangent must consequently have and there. But , so smoothness forces . The arc-length identity also illustrates the alternatives: prevents reaching either zero with real , while gives a nonhorizontal limiting meridian and a conical singularity.
Now . On the connected interior, has one fixed sign because . Therefore , and
The revolved surface is the unit sphere centered at , with only its two poles omitted. Those points are antipodal. This proves the claim using smooth endpoint criterion for a surface of revolution, without integrating a general square root.
No. The missing point is not assumed to complete as a smooth surface, so the hypotheses of the global Gauss-Bonnet theorem do not apply to .
For a concrete counterexample, rotate a smooth simple arc , parametrized by arc length for , about the -axis. Arrange that it starts smoothly on the axis,
stays in for , and converges to another point of the axis as , with
The endpoint is omitted. The resulting surface of revolution is diffeomorphic to minus one point, and adjoining its limiting endpoint makes the set compact.
For an arc-length surface of revolution,
Therefore the total Gaussian curvature of a punctured surface with a singular compactification point is
which can take values different from . Compactness of the one-point closure alone therefore does not determine the integral.
No. Fix and, near , let
Then , so this is a regular unit-speed profile with on a sufficiently small interval. Rotate it around the -axis. For an arc-length surface of revolution, , and therefore
At , the formulas from part (a) give the principal curvatures
They are unequal because , so the point is not an umbilical point. Every point of a sphere is umbilical. Consequently no neighbourhood of this point can lie on a sphere, giving a non-spherical surface of constant Gaussian curvature one.
The curve is symmetric in both coordinate axes and under interchange of and . Its shape, including its eight inflection points, is:
Writing , the surface of revolution has equation
Let
Its gradient is
If this vanished, then and , but at such a point , not five. Hence zero is a regular value, and the regular level set theorem shows that is a smooth embedded surface.
For a surface of revolution, the two principal curvatures are the curvature of the meridian and the normal curvature of a parallel. Along ,
so the normal is vertical in the meridian plane and the parallel principal curvature vanishes. Therefore the Gaussian curvature, the product of the principal curvatures, is zero there.
These are not the only zero-curvature points. The meridian itself has inflection points, at which its principal curvature vanishes. Setting and , their positive squared coordinates satisfy
Besides interchanging and , the solution is approximately
Each corresponding meridian inflection point sweeps out another circle on , so does not exhaust the zero set of the Gaussian curvature.
With
the coordinate tangent vectors satisfy
Thus the first fundamental form is
Geometrically, is the half of a helicoid with positive radius, winding upwards indefinitely.
Consider the upper half of the catenoid, parametrized as the surface of revolution
It has the same first fundamental form, so defines a local isometry. By the invariance of Gaussian curvature under local isometry, the curvatures agree; directly, the conformal metric above gives
The plane
meets the one-sheet hyperboloid in the two disjoint curves
They are the two opposite meridians of the surface of revolution. Parametrize the generating profile by arc length. Its acceleration lies in the meridian plane and is orthogonal to the profile tangent; it is also orthogonal to the azimuthal tangent. It is therefore normal to the surface, so both meridians are geodesics. This is the disjoint case in plane-section geodesics of the unit one-sheet hyperboloid.
Write , , , and let be the first fundamental form. Since
differentiating and , or equivalently taking the two inner products of the second formula with , gives
The matrix is invertible because is a regular embedded surface parametrization. Consequently the two geodesic equations hold exactly when is orthogonal to both tangent vectors and , which says precisely that is a normal vector. This is the ambient acceleration criterion for a surface geodesic.
Because is tangent and is normal,
Thus an affinely parametrized geodesic has constant speed, as recorded by constant speed of an affinely parametrized geodesic.
For a surface of revolution, use profile arc length and azimuth . Its Riemannian metric is
The azimuth is an ignorable coordinate, so the corresponding geodesic equation has the first integral
If and is the oriented angle with the parallel, then the component of velocity along the parallel is
Since is constant,
This is the Clairaut first integral for a surface of revolution.
A plane has both principal curvatures zero, hence . A circular cylinder of radius has principal curvatures and , hence
Because the absolute value of mean curvature is preserved even if one reverses the chosen orientation, no Euclidean motion can carry any open piece of the cylinder to an open piece of the plane. Thus the condition does not characterize planar pieces.
There are analogous examples for both signs of constant Gaussian curvature. Start with the arc-length surface of revolution
On a sufficiently small interval about , this is a regular surface and the curvatures of an arc-length surface of revolution give
At its mean curvature is
For this is a piece of the unit sphere and , whereas for it equals . By continuity, sufficiently small pieces around their central circles have disjoint ranges of , so no pieces in those chosen neighbourhoods are related by a Euclidean motion.
For curvature minus one, use
again on a sufficiently small interval. Then
The choices and give and . Restricting to small enough pieces again separates the ranges of . The constant Gaussian curvature surfaces of revolution therefore supply the requested noncongruent examples for and .