Work first on the unit sphere. A spherical lune of angle has area : its fraction of sphere area is . The three great circles extending the sides of a nondegenerate spherical triangle divide the sphere into four antipodal pairs of triangular regions. Call the desired region , of area , and its three adjacent regions , of areas . These four regions contain one region from each antipodal pair, so . The lune at each vertex consists of and one of these adjacent regions. Therefore, if the three interior angles are ,
which proves the spherical excess formula, the spherical-triangle form of the Gauss-Bonnet theorem:
For a sphere of radius , multiply this area by .
Triangulate a convex spherical -gon by diagonals from a vertex. There are spherical triangles, and their angles add to the polygon's interior angle sum. Thus its unit-sphere area is
For a nondegenerate convex regular polygon in an open hemisphere, area is positive and each angle is less than , giving . Every angle in this interval occurs. Indeed place vertices at equal longitude spacings and colatitude about a pole, and join consecutive vertices by shorter great circle arcs. The polygon is convex and regular. Split a central isosceles spherical triangle along the perpendicular to its edge. The resulting right spherical triangle has angles , , , and hypotenuse . The angular spherical law of cosines yields
so . As increases from to , increases continuously through exactly
The endpoints are degenerate limits, not strict convex polygons.
For the spherical triangle reflection group, positive area requires . Each angle is less than , so the integer denominators are at least two. Arrange . If the sum is at most one, hence . If the sum is again at most one; thus either and any works, or and . These triangles exist, for example as the reflection chambers of a regular dihedral configuration, tetrahedron, cube, and dodecahedron, respectively.
To count group elements using the assumed tessellation, first label the original triangle's three vertices by their types and propagate these labels through side reflections. Around a type- vertex there are sectors; the associated alternating reflections make a full turn and return the labels unchanged. The same holds at the other types. Every closed path in the dual tessellation is generated by these circuits around vertices, since the sphere is simply connected. Thus the labels are globally consistent, including when two angle denominators coincide. Every generated isometry preserves these labels. An element stabilizing a triangle therefore fixes its three vertices and is the identity. Consequently group elements correspond bijectively to triangles, and area gives
The possibilities, including permutations of the entries, are
Here is an explicit dodecahedron construction for the last case, avoiding an assumption about which vertices of the tessellation to join. Put , and take the convex hull of the twenty points
with independent signs. They all have squared radius three. The supporting plane contains the five vertices
in cyclic order. Consecutive distances are , and nonconsecutive distances are , so this is a regular pentagon. Changing the two signs in its normal and cyclically permuting coordinates gives twelve supporting planes, all with a congruent pentagon. Each listed vertex lies on three of these faces; the sixty face-edge incidences pair into thirty edges. The faces form a closed convex polyhedral surface with , hence exhaust the boundary of the convex hull. This constructs a regular dodecahedron.
Choose the spherical directions of a face center , the midpoint of its edge between , and that edge's endpoint . Normalize these to the unit sphere. The three side planes of triangle are , , and with . Their reflections are coordinate sign changes in the first two cases and
in the third, since . Substitution in the twenty listed vertices, using , shows that all three reflections permute the vertex set. The side-plane angles give interior angles at , at , and at because and . Thus this triangle is congruent to , and its side-generated group is , conjugated by the aligning isometry.
Figure 1.
Regular dodecahedron and its face-center, edge-midpoint, vertex spherical reflection chamber
. Details.
It already has elements. Conversely, a symmetry of the dodecahedron is determined by the image of one face, one vertex on that face, and the orientation along its boundary: there are at most choices. An isometry fixing these choices fixes that face pointwise and must preserve the polyhedron's interior side, hence is the identity. Therefore the complete symmetry group of the constructed dodecahedron is , including orientation-reversing symmetries.
Because the events are pairwise disjoint events, their count can only be zero or one. The event that the count is zero is the complement of an event of their union. Finite additivity therefore gives
Now use for the fixed number of independently located ships. Normalize the radius to one and write their positions as unit vectors . A point on the sphere is reached by ship precisely when , so each ship reaches an open hemisphere. Coverage fails exactly when there is a unit vector with for every . Equivalently, all ship positions lie in some closed hemisphere.
With probability one no pair of ship vectors is antipodal and no three are linearly dependent: the exceptional choices lie on sets of zero surface area. For such a configuration, containment in a closed hemisphere implies containment in an open hemisphere. To see this, choose its inward normal , so . At most two vectors lie on its boundary. If there are two, their sum has positive dot product with each, since they are not antipodal; if there is one, use that vector itself. Perturb slightly in this direction. The boundary dot products become positive while all already positive dot products remain positive. Thus the strict and non-strict containment conditions have the same probability here.
Condition on the unoriented axes . Choose representatives by any fixed sign convention. By uniform sampling and independence, the actual positions are with independent fair signs . Conditional on these axes, each of the sign choices has probability .
The great circles partition the sphere into open regions. In each region the sign vector is constant. No sign vector labels two different regions: its strict inequalities define a convex cone, and normalized line segments within that cone connect any two points of its spherical section. The regions of a general-position great-circle arrangement therefore yield exactly realized sign vectors.
The chosen positions lie in an open hemisphere if and only if some has for every , that is, for every . Failure of coverage thus corresponds exactly to one of the realized sign choices. These choices are mutually exclusive events, each of conditional probability , so the first part applies:
The result is independent of the axes. Averaging gives the coverage of a sphere by random open hemispheres:
For this is zero; for it is . If no ship lands, coverage has probability zero separately. The counting uses equiprobable orientation signs, not an assumption that the spherical regions have equal area.
A geodesic is an affinely parametrized curve satisfying for the Levi-Civita connection of the Riemannian metric. In coordinates, write . For a vector field along the curve,
Putting gives the geodesic equation
This is a smooth second-order ordinary differential system, so the Picard-Lindelöf theorem gives local existence and uniqueness for prescribed position and velocity.
To prove local extension of geodesic velocity, first suppose . The constant curve through solves this initial value problem, so uniqueness makes constant locally. The zero vector field is the desired extension.
Otherwise choose a chart about in which the first component of the coordinate velocity is nonzero. Write the coordinate curve as and define
At its derivative has columns and is invertible, because the first component of is nonzero. The inverse function theorem therefore supplies coordinates on an open neighbourhood after shrinking the parameter interval to . Along the curve these coordinates are . The smooth coordinate field , pushed back through and the original chart, agrees with . This proves the extension without assuming that a long geodesic has no self-intersections.
By metric compatibility, differentiation along the curve gives
The local extension above permits the ordinary vector-field version of the metric identity to be used along the arc, or the same identity follows directly from the coordinate derivative. Hence an affinely parametrized geodesic has constant speed, including the zero-speed case.
Now let be the unit sphere in . Its induced Levi-Civita derivative is the tangential projection of the ordinary ambient derivative: projection preserves the metric identity, and the commuting ambient coordinate derivatives give zero torsion. By uniqueness of the Levi-Civita connection, proved in Question 5, this is the induced connection.
Thus a curve on the sphere is a geodesic exactly when its ambient acceleration has no tangential component. The normal space is spanned by , so . Differentiating twice gives and
where is the constant speed. Therefore . With initial data and , all solutions are
and, when , . The orthogonality and length conditions show directly that the displayed curve remains on the sphere, and its acceleration is , so it is indeed a geodesic. The nonconstant geodesics are the great circles traversed at any constant speed; arbitrary parameter intervals give their restrictions, and shifting the initial parameter simply shifts the formula. There are no other geodesics.
Use the unit sphere , its north pole , and the equatorial complex plane . The line from the north pole to a sphere point meets that plane at
The north pole maps to . The inverse stereographic projection is
The antipodal point has coordinate . Since , this is when both sides are finite and nonzero. Zero and infinity correspond to the two poles and are exchanged by the same extended convention. The inverse formula also proves the converse, giving the antipodal stereographic coordinate relation
The requested rotation result is that sphere rotations correspond exactly to Möbius transformations
The matrices form , and opposite matrices induce the same transformation. Thus the rotation group is identified with . This is the sphere rotations as special-unitary Möbius transformations result, which need not be proved here.
For a planar circle , and , substitute and . Multiplication by gives the circle-plane relation under stereographic projection:
The lift lies in this plane, and conversely its intersection with the sphere projects onto the circle. It is a nondegenerate circle on the sphere. The north pole is not on the displayed plane, since substitution there gives two rather than zero.
A great circle is the intersection with a plane through the sphere's centre. Here this holds exactly when
The unit circle lifts to the equator. If a different circle lifts to a great circle, its plane and the equatorial plane are distinct planes through the origin, so their intersection cuts the sphere at two antipodal equatorial points. Their planar coordinates are and on .
Conversely, if the planar circle meets the unit circle in and , their lifts are antipodal equatorial points. The plane of the lifted circle contains their midpoint, the origin, so that circle is great. Equivalently, adding and gives . The exclusion of the unit circle ensures the two intersection points are a genuine pair rather than coincident circles. This proves the antipodal equatorial intersection criterion for a great circle.
Use suffix notation, summing repeated indices from one to three. The contraction identity for the Levi-Civita symbol gives
Here because is a unit vector. For the second cross product identity, use :
The first term vanishes because is symmetric while the Levi-Civita symbol is antisymmetric in those indices. The last equality uses cyclicity and antisymmetry of the scalar triple product.
On the unit sphere, a great circle has radius one, so the spherical distance is its shorter arc length, equal to its central angle in . The dot product of its endpoint unit vectors is the cosine of that angle. Hence
For the angular formulas, take the ordinary nondegenerate convex minor spherical triangle: no pair of vertices is antipodal and the three vertices do not lie on one great circle. These are needed for the displayed denominators and interior angles to be defined. Merely requiring three distinct points, as the PDF does, does not exclude degeneracy.
Put , and . The outgoing unit tangent vectors at are
Their dot product is . Equivalently, they are obtained from the normalized plane normals and by the same right-angle rotation in the tangent plane: , and similarly for . Rotation preserves the dot product, giving
Since and , the first proved identity becomes the spherical law of cosines:
For the spherical law of sines, take norms in the second proved identity. Writing , and using , gives
Cyclic permutation gives the corresponding formulas at and . Dividing each by the positive product proves
Finally, if all sides equal , the spherical law of cosines gives
because makes and . Cosine is strictly decreasing on , so every angle of a nondegenerate equilateral spherical triangle is greater than .
For stereographic projection, choose the north pole of the unit sphere and identify the plane with the complex plane by . Project a point along the line joining it to ; adjoin for the north pole to identify the whole sphere with the Riemann sphere. A point of that line is . Its last coordinate vanishes when , giving
Using , or solving this line's second intersection with the sphere, gives the inverse
A great circle lies in a plane through the origin. Its projected equation is
It is a straight line only if , meaning the plane contains the north pole and the south pole. Thus if all three sides of a nondegenerate spherical triangle projected to straight sides of a Euclidean triangle, all three distinct side planes would contain both poles. Each pair of side planes could then meet on the sphere only at those same two poles, which cannot supply three distinct triangle vertices. A nondegenerate spherical triangle cannot project to a Euclidean triangle. If a side passes through the projection pole, its image is unbounded and also cannot be a finite triangle side.
A nonidentity rotation in three dimensions has an axis through the origin: an orthogonal three-by-three matrix of determinant one has an eigenvalue one, since nonreal eigenvalues pair as conjugates, real eigenvalues are , and their product is one. Its axis meets the unit sphere in an antipodal pair, which is fixed. In the identity case every point is fixed, so an antipodal pair can again be selected. Projecting and gives
whenever both points are finite. Thus the associated Möbius transformation fixes an antipodal pair satisfying the claimed relation. The universally valid relation is on the Riemann sphere, with and paired. A rotation about the projection axis fixes exactly that pair, so the PDF's literal finite product needs this extended-coordinate convention. This is the antipodal stereographic coordinate relation.
For a polygonal cell decomposition of the sphere, Euler characteristic gives
Count incidences between faces and edges. Each edge borders two faces, and each face has at least three sides, so . If every vertex had valence at least six, counting edge endpoints would also give . Hence and , implying , contrary to Euler's formula. Thus some vertex has valence less than six.
There is a missing qualification in the printed affine-line conclusion. Two distinct parallel lines have no intersection point, so its intersection condition holds vacuously, but they do not meet at a finite point. Even three or more distinct parallel lines give the same counterexample. Consequently that conclusion is false literally without a restriction on parallel lines.
Here is the intended spherical argument when the lines are pairwise nonparallel. Lift each line in the plane to the plane through it and the origin in ; intersect these planes with the unit sphere to obtain great circles. A common axis of all these planes meets in the required common point. Suppose no such axis exists. Their circle arrangement then decomposes the sphere into polygonal faces with at least three edges. To see why a two-sided face is impossible, its two great-circle edges would have antipodal endpoints. Every defining hemisphere containing that face would contain both endpoints and would therefore have its boundary plane through their axis, contradicting the absence of a common axis.
Every circle-arrangement vertex corresponds to an intersection of lifted planes. Because no two affine lines are parallel, this axis meets , so the vertex corresponds to a finite intersection of the original lines. By the assumed multiplicity, at least three circles pass through it, giving valence at least six. This contradicts the preceding sphere count, proving concurrence in the nonparallel case. It is the ordinary vertex in a nonconcurrent great-circle arrangement argument.
Alternatively the corrected projective statement allows parallel lines, but requires the intersection condition at infinity as well, and concludes concurrence at a possibly infinite projective point. The same great-circle proof applies; concurrence at infinity represents a parallel family. The printed condition about finite affine intersections alone must not be used to assert a finite common point for such a family.
We use , whose spectrum on a compact manifold is nonpositive; write for the positive Laplace-Beltrami operator. This convention will also make the heat operator in Question 3 equal to .
Let be an orthonormal basis of , and let be the unit-speed geodesic with and . Since a geodesic has vanishing acceleration for the Levi-Civita connection, differentiation twice along it gives the Riemannian Hessian:
Taking its metric trace yields the geodesic trace formula for the Laplace-Beltrami operator
The positive-sign convention puts a minus sign in front of this sum.
For the unit sphere, take and tangent unit vectors orthogonal to . Its great circle geodesics are . For a smooth ambient function near the sphere, the ordinary chain rule gives
The ambient orthonormal basis is . Thus, writing and similarly for ,
This proves the ambient restriction formula for the spherical Laplacian and shows why ambient derivatives normal to the sphere must be subtracted. The equivalent formula in spherical coordinates is
Let be the vector space of homogeneous polynomials of degree in variables, and its harmonic polynomials. If , homogeneous polynomial scaling gives . Substitution into the spherical coordinates formula gives
The restrictions are the degree- spherical harmonics. A homogeneous polynomial vanishing on the sphere vanishes on every nonzero ray and hence identically, so restriction is injective on .
We prove the harmonic decomposition of homogeneous polynomials that both counts these eigenfunctions and establishes completeness. For an ambient harmonic homogeneous polynomial of degree and , the spherical coordinates formula gives
For its coefficient is nonzero. Inductively assume homogeneous polynomials of degree have been decomposed into sums of . Apply this decomposition to for , and lift each summand by multiplying by and dividing by the displayed nonzero coefficient. The resulting satisfies , so . The same coefficient formula shows that no nonzero element of can be harmonic. Starting at degrees zero and one therefore proves the direct decomposition
Since , the multiplicity is
where the second term is zero for .
On , iterating the decomposition writes every polynomial restriction as a finite sum of spherical harmonics. The Stone-Weierstrass theorem makes these polynomial restrictions dense in , since coordinate functions separate points and constants are included; they are consequently dense in . Integration by parts makes symmetric on smooth functions and gives orthogonality between distinct eigenvalues. Normalizing within each finite-dimensional eigenspace gives a complete orthonormal eigenbasis . To check the full operator spectrum, let . For smooth , integration by parts gives the coefficients of as . Therefore finite harmonic partial sums approximate both and in , hence approximate in the graph norm. Conversely every coefficient sequence with is the graph norm limit of its finite harmonic sums. Thus the closure of has exactly this operator domain and is the real diagonal self-adjoint operator with entries . If is not one of these entries, the inverse has entries and is bounded because . This proves that there are no missing spectral values. The spectrum of the Laplacian on a sphere is
with the above multiplicities; for , negate every eigenvalue. For example has eigenvalues , with multiplicities one at zero and two for , and has multiplicity . The zero-dimensional sphere consists of two isolated points and has only the zero eigenvalue, with multiplicity two.
Take the normalization
The first variation of geodesic energy says that the critical points on the fixed-endpoint path space are exactly the affinely parametrized geodesics. The kernel of the second variation of geodesic energy, or Riemannian index form, is the space of Jacobi fields vanishing at both endpoints. Hence a geodesic is a nondegenerate critical point exactly when that space is zero, or equivalently when its terminal endpoint is not a conjugate point to its initial endpoint along the given geodesic.
The Morse index theorem states that the index is the sum of the multiplicities of all conjugate points strictly inside the parameter interval:
The multiplicity at the terminal endpoint gives nullity rather than an additional contribution to the index. These statements use the usual Sobolev completion of the path space; smooth paths have the same homotopy type.
First suppose as well as , and put . There is a unique great circle through these two points. Every critical path runs along it with constant speed, possibly passing around it extra times. If
then a complete enumeration without repetitions is
Its length is . Equivalently the two positive length lists are
There are no other critical paths, because a nonconstant geodesic of the round sphere is a constant-speed great circle and its plane must contain .
To compute conjugate points and indices of round-sphere geodesics, the round unit sphere has constant sectional curvature . Along a geodesic of speed , a normal Jacobi field in a parallel direction satisfies . A field with is therefore a constant multiple of in each of the normal directions. Its tangential component satisfies and contributes no endpoint-vanishing field. Consequently the conjugate points occur at , each with multiplicity . Since neither length list contains an integer multiple of , all the displayed critical paths are nondegenerate, and the Morse index theorem gives
The permitted case requires separate treatment. There is a constant geodesic, which has index and nullity zero. All other critical paths are
For each , this is a family parametrized by ; both directions of traversal are included through and . The interior conjugate points number , and the endpoint is also conjugate. Thus
These are Morse-Bott critical manifolds for , rather than nondegenerate critical points. For the same formulas give zero index and nullity, with the two isolated directions comprising .
For the requested homology calculation, choose distinct nonantipodal endpoints. Concatenation with a fixed path back to the basepoint gives a homotopy equivalence between this fixed-endpoint path space and the based loop space . We use the Morse cell-attachment theorem for geodesic energy: on a complete compact Riemannian manifold, the fixed-endpoint energy, when all its critical points are nondegenerate, gives a CW complex of the same homotopy type with one cell of dimension equal to the index of each critical point. One can obtain this theorem from finite-dimensional broken-geodesic approximations and ordinary Morse theory; critical energy values tend to infinity here.
The two index lists interleave to give exactly one cell in every dimension , . If , these dimensions are separated by at least two. The cellular homology groups therefore have zero boundary maps, since no occupied cell dimension has an occupied dimension one lower. With integer coefficients,
This determines the graded abelian groups. The argument does not need an identification of the multiplication on loop-space homology.
Finally apply the Freudenthal suspension theorem: for an -connected based CW complex , , the suspension homomorphism
is an isomorphism for and a surjection for . A sphere is -connected, and its reduced suspension of a topological space is homeomorphic to . Hence
The isomorphism is the suspension map. Its stable range is also reflected by the Morse theory cell structure of : after its bottom -cell, the next positive-dimensional cell has dimension . For the stated homology problem , all the connectivity hypotheses apply.
Use azimuth measured from north toward west, and positive hour angle westward. These conventions are forced by the signs in the coordinate formulae. In the diagram the observer is at , the local vertical meets the celestial sphere at the zenith , and the north celestial pole is . The astronomical horizon is perpendicular to ; the celestial equator is perpendicular to . Their intersections with the celestial meridian give the north horizon point and the upper equatorial meridian point.
Figure 1.
The celestial sphere with horizon and equatorial coordinates
. Details.
The north celestial pole has altitude ; thus the angle between and is . Project along its vertical great circle onto the astronomical horizon at : the arc is the altitude , and the westward horizon arc from north to is the azimuth . Project along its hour circle onto the celestial equator at : the arc is the declination , and the westward equatorial arc from the upper celestial meridian to is the hour angle . Equivalently the triangle on the celestial sphere has sides , and . All five angles refer to arcs on their specified reference circles, not arbitrary angles in the projected drawing.
Write for one sidereal day in minutes and . An equatorial star at an equatorial site rises along a vertical great circle, passes through the zenith, and descends on the opposite side. Its azimuth changes by at the crossing. The restricted altitude travel prevents following it continuously by rotating over the zenith.
The maximum azimuth rate is radians per minute, so the shortest half-turn takes minutes. During that lost-track interval the star moves through
For minutes this is approximately ; using a 24-hour day gives . If the quoted zenith blind spot size means the angular radius of a symmetrically placed crossing gap, it is , approximately .
This derives the ideal crossing-gap size with instantaneous acceleration and an available altitude drive. It does not uniquely define a circular forbidden region for all nearby trajectories. For example, at an equatorial site a star of small nonzero declination has maximum azimuth rate at transit: its minimum offset is constrained by . That rate contour and the half-turn crossing gap are different definitions of a zenith blind spot. Actual tracking footprints also depend on acceleration and the reacquisition strategy, as discussed in the telescope designers' tracking discussion.
The length of a curve is . Its arc length parameter is . Regularity gives , so the inverse function theorem gives a smooth inverse and has .
Reparametrize a length minimizer to constant speed on and use the energy functional . By Cauchy-Schwarz inequality, every competitor has , with equality for constant speed, so this parametrization also minimizes . For a fixed-endpoint variation with tangential vector field , differentiation and integration by parts give
The boundary term is zero. Arbitrary smooth tangential of compact interior support are realizable by the stated variation fact. Taking to be a nonnegative cutoff times proves . Hence a length minimizer is a geodesic after constant-speed reparametrization. The original parameter need not be affine: arbitrary varying-speed parametrizations preserve length but have nonzero covariant acceleration. This qualification is necessary for the literal wording.
For distinct nonantipodal on the punctured unit sphere, there is a unique shorter great circle arc, of length . A minimizing curve exists exactly when that shorter arc avoids the removed north pole. If it avoids the pole it attains the spherical lower bound. If it passes through the pole, arbitrarily small smooth detours have lengths tending to , but equality would force the unique shorter arc, which is unavailable. Thus the infimum is not attained; the longer great circle arc is not a substitute minimizer.
For antipodal in the punctured sphere, one can choose a great circle semicircle avoiding the north pole; it attains length . Thus every admissible antipodal pair has a minimizer. If identical endpoints are included despite the earlier distinctness stipulation, the infimum is zero, but no smooth regular curve attains it; only a nonregular constant curve does.
The great circle containing the pointing and celestial pole is the intersection of the unit sphere with the meridian plane . The orthogonal projection of onto that plane, normalized to unit length, is
Within the local meridian chart , its declination is therefore . Outside that chart, the same construction gives an oriented great circle parameter; the foot can lie on the opposite right-ascension half of the meridian, and need not be its ordinary declination.
To verify the right angle geometrically, the tangent to the great circle from toward is proportional to . Since , that tangent has only a component. The tangent from toward the pole, , lies in . Their orthogonality proves the claimed spherical right angle. Thus within the local meridian chart, is the declination of the perpendicular foot on the pointing meridian.
There are antipodal perpendicular feet on the complete great circle. On the local meridian chart, the telescope field selects the foot near the pointing; the cotangent equation alone determines only modulo . At a coincident foot or pole, the corresponding angle is understood by continuity rather than by a nonzero tangent vector.
Use the gnomonic projection associated with an undistorted focal plane. Write and rotate the celestial Cartesian coordinate system so that the pointing meridian has longitude zero. The stellar direction and an orthonormal basis adapted to the optical axis are
Here points east and points north. Intersect the ray with the plane . It gives , so the detector coordinates are
These equations also avoid spurious singularities caused by writing individual tangents or cotangents.
To put this gnomonic projection in the desired form, let and choose locally by
Thus . The denominator becomes , the numerator for becomes , and . Consequently
Use the local meridian chart , with chosen continuously near and at the image centre. A visible gnomonic projection requires , but this front-hemisphere condition alone does not select that meridian chart. A narrow field near a celestial pole can cross the opposite meridian; for such fields use the Cartesian expressions above and distinguish the oriented great circle parameter from ordinary declination. In particular, the small-field limit is and , with angles in radians. The factor is the shrinking angular distance per unit right ascension near the pole.
A plane through the origin has equation for some nonzero normal . Dividing that normal by its Euclidean norm makes without changing the plane. Substitute the spherical coordinates from (a) and cancel the nonzero radius:
Its intersection with the sphere is the desired great circle; changing the sign of all three coefficients describes the same circle.
At the first endpoint, the Cartesian coordinates are , so its great circle must have . At the second endpoint, the plane condition gives . Since , an equivalent regular plane equation is
Where , divide by to obtain
The regular implicit equation includes the equatorial first endpoint; the tangent form is undefined there and must be read by a limit. The shorter connecting arc of this great circle is the shortest path. The endpoints are not antipodal, so this shorter arc is unique. For example, the central angle is , giving spherical distance .
Length functional. On the unit sphere, write the position vector in spherical coordinates as
Its two coordinate tangent vectors satisfy , and . Consequently the induced Riemannian metric is . On a segment for which increases and ,
Segments where is not monotone require another parameter or a subdivision. Endpoint turning points can be handled by a limit.
First integral. With , there is no explicit dependence. The Euler-Lagrange equation therefore says that
is constant. For , put and solve:
The radicand must be nonnegative along the chosen segment. The printed expression with both limits fixed at describes a longitude difference between endpoints; a formula for needs the variable upper limit and the additive constant shown here. The case gives a meridian with constant longitude. The equator is also a stationary route, although it cannot be parameterized using changing .
Integration and geometric meaning. Put , so and
For a nonconstant segment , and writing , the integral becomes
Rearranging, and absorbing phase and sign into two constants, gives
Multiplying by shows that the corresponding Cartesian coordinates satisfy . Thus every such stationary route lies in a plane through the sphere's center: it is a great circle, the geodesic of the sphere. The meridians and equator are the limiting or separately parameterized cases of the same description.
Rome to Singapore. Use exactly the approximate coordinates supplied in the question: at departure and at arrival. Inserting them into the preceding relation determines
Indeed the right side is one at Rome and zero at Singapore. This corresponds to , . In latitude , the route is : it starts at north with an initially eastward heading and then curves southward to the equator. The first-integral expression in has an integrable endpoint singularity at departure, where has a turning point; the longitude parameter is regular there.
Figure 1.
Shortest spherical route for the approximate Rome and Singapore coordinates in the question
. Latitude versus longitude for the derived great circle, with endpoints at 45 degrees north and 15 degrees east, and zero degrees north and 105 degrees east. The quarter-circle parameter increases uniformly in spherical distance. Details.
For an explicit regular arc-length parametrization, let and . Their dot product is . Hence
Both and equal one. The shorter great circle arc is the global shortest path: for any unit-speed curve from , its central angle satisfies by the Cauchy-Schwarz inequality, since the tangential projection of has length . Integrating gives length at least the endpoint angle , which this route attains. For a sphere of radius , the corresponding shortest distance is .
Use arc length as the affine parameter, and put a dot over derivatives with respect to . The geodesic Lagrangian on the sphere is
The cyclic coordinate gives . With the constant normalized as in the paper,
Here has units of inverse length, because is physical arc length. Unit-speed normalization gives
For , division by yields the spherical-geodesic first integral
The turning latitudes satisfy . In the usual polar-coordinate range ,
The maximum departure from the equator, often the geometric quantity intended by an angular amplitude, is instead
Thus polar angle and signed latitude must not be interchanged. At the geodesic is the equator. At it is a meridian through the poles; cannot serve as a global parameter and the divided equation is inapplicable. The limiting polar range is then .
The original PDF prints an ambiguous derivative with the square on rather than a conventional derivative notation. If the intended equation was second order, differentiating the first integral, or eliminating from the Euler-Lagrange equation, gives the equally useful form
It has the same normalized geodesics and the same turning angles. Giving both forms resolves the typographical ambiguity without pretending that a second derivative is the square of a first derivative. Geometrically these trajectories are great circles, with inclination to the equator.
For great circles on a sphere, with no coincident circles or triple intersection, the number of open regions is . The first circle gives two regions. Each subsequent circle meets the previous circles at distinct points and is divided into that many arcs, each splitting a previous region. Summing the increments proves the formula. If the circles are , each region has one fixed sign vector . Conversely a realized strict sign vector has a connected region: its cone is an intersection of open half-spaces, and radial projection of line segments connects any two points.
Riemannian geometry Created 2026-09-24 Updated 2026-10-14
Riemannian geometry studies smooth manifolds equipped with a Riemannian metric: an inner product at each tangent space, varying smoothly with position. This local measuring rule determines angles, arc length, Riemannian distance and geodesics. An inhabitant of a surface can discover its geometry by measuring within it, without knowing how it sits in a larger Euclidean space.
A circular cylinder is a particularly useful example. Its surface bends in space, yet unrolling it preserves the induced metric: a small patch has the geometry of a flat sheet. By contrast, a round sphere has positive Gaussian curvature. The distinction between intrinsic flatness of a circular cylinder and extrinsic curvature separates the geometry an inhabitant measures from the way an outside observer sees the surface bend.
Geodesics supply the analogue of straight lines. On a round sphere they follow great circles; on a circular cylinder they become straight lines when lifted to an unrolled sheet. Their arc length lets us compare candidate routes, as in great-circle distance and Riemannian distance on a circular cylinder. The same measuring rule also defines differential operators such as the Laplace-Beltrami operator, connecting geometry with diffusion and spectral geometry.
Bernhard Riemann's 1854 inaugural lecture proposed studying spaces of arbitrary dimension through their infinitesimal measuring rules, including a positive quadratic expression for the squared line element. This moved the subject beyond a particular surrounding space: the measuring rule itself became part of the geometry. [ref].