Colatitude Created 2026-10-20 Updated 2026-11-05
Colatitude is the angle from the positive polar axis, usually denoted with . On a sphere it complements latitude : . Thus the north pole, equator and south pole have colatitudes zero, and .
With longitude , the standard spherical coordinates are , , . The surface element is , which shows why an integral over the sphere must include the sine weight. Some disciplines exchange the names of and , so formulas should accompany symbol conventions.
Euler angular velocity vector 2026-10-20
Relative angular velocities add as vectors: . Geographic pole latitudes and longitudes must first be converted into Cartesian vector directions.
Longitude Created 2026-10-20 Updated 2026-11-05
Longitude is an angular coordinate around a chosen polar axis, measured from a reference half-plane. On Earth the conventional reference is the Greenwich meridian. In a Cartesian coordinate convention it is , with a specified range such as .
Together with latitude and a radius it describes a point using spherical coordinates. Longitude is undefined at the poles because every meridian meets there. Its numerical jump at the chosen meridian cut is a coordinate discontinuity, not a discontinuity of the sphere itself. On an oblate reference ellipsoid, geographic latitude needs an additional geodetic convention.
Let point to the equatorial meridian at zero longitude, to the equator at E, and to the north pole. Use a right-hand positive Euler angular velocity vector. Relative rotations add as vectors, not as geographic coordinates:ConsequentlyHere is the longitude of the positive Euler pole, and its latitude is zero. The antipodal pole with the opposite angular-velocity sign is an equivalent convention; mixing a pole reversal with an unchanged sign would give the wrong motion.
At latitude and longitude , . Motion is . A meridian boundary has horizontal normal , so its across-boundary velocity isFor a transform fault this must vanish along the whole meridian, not only at an isolated point. Thus . Select the solution in the western hemisphere:The other solution is the antipodal meridian in the eastern hemisphere. Geometrically, the transform meridian is in a great-circle plane perpendicular to the Euler angular velocity vector. Its outgoing tangent direction at either pole, expressed in the fixed axes, is .
For an open cover , the Mayer–Vietoris theorem gives the long exact sequenceIt ends in . To prove it, let be the subcomplex generated by singular simplices lying wholly in or wholly in . There is a short exact sequence of chain complexesExactness follows from the singular-simplex bases: the intersection of the two chain subgroups consists exactly of simplices lying in both sets. The small-chain locality theorem for singular homology says the inclusion of this small-chain complex into induces an isomorphism on homology; barycentric subdivision is its standard justification. The long exact sequence of a short exact sequence of chain complexes now proves the theorem. For a homological cycle represented as , the connecting map is , since lies in the intersection. This also identifies the displayed maps and their signs.
For the glued solid tori, use open collar enlargements of the two halves. Each retracts to a circle; the overlap retracts to their boundary torus. Thus the halves have and higher homology zero, while the overlap has and . In the overlap choose longitude and meridian generators. The meridian bounds a disk in each solid torus and the longitude generates each first homology, so the map on isIts kernel is the meridian copy of and its cokernel is . The map on is the injective map . Exactness therefore gives and . The preceding segment is , giving . Connectedness gives , and all higher groups vanish. HenceAs a geometric check, the identity boundary gluing identifies the product with .