The classification of compact surfaces states that every compact connected topological surface without boundary is homeomorphic to exactly one of the sphere, a connected sum of surfaces consisting of tori, or a connected sum of real projective planes. The torus family is orientable and the projective-plane family is nonorientable; their respective genera are unique. Including makes the sphere the genus-zero orientable case. If boundaries are allowed, the number of removed open discs is an additional invariant.
A finite subdivision into vertices, edges and polygonal faces defines the Euler characteristic
Count cells after all identifications. Subdividing an edge adds one vertex and one edge; splitting a face adds one edge and one face. Each operation leaves unchanged. Comparing subdivisions through a common refinement proves independence of the subdivision.
For the connected sum of surfaces, remove an embedded open disc from each surface and identify the resulting boundary circles by a homeomorphism. The resulting closed connected surface is denoted .
Removing a disc decreases the Euler characteristic by one. Gluing the remaining surfaces along their common boundary subtracts the characteristic of a circle, which is zero. Thus
This can be verified by choosing matching subdivisions of the boundary circles and counting the vertices and edges identified in the gluing.
A square model of the torus has one vertex, two edges and one face, so its Euler characteristic is zero. The connected-sum formula gives
The real projective plane has a bigon model with one vertex, one edge and one face, hence characteristic one. Therefore
Take , and . The first is orientable, while , the Klein bottle, is not, so and are not homeomorphic.
Both and are nonorientable and have Euler characteristic . By the classification of compact surfaces, both are homeomorphic to the connected sum of three projective planes. Hence
This is failure of cancellation for connected sums of surfaces.
For a nonconstant holomorphic map of degree between compact connected Riemann surfaces, the Riemann-Hurwitz formula is
Here is the local degree, characterized by local coordinates in which the map is . The sum is finite and its terms are nonnegative; a ramification point has .
If , the Riemann-Hurwitz formula gives , where . If , the right side is nonpositive, a contradiction. Therefore
The given Weierstrass elliptic function is even, by replacing the lattice index with . Differentiation gives
For any , reindexing the sum shows . Thus is constant off the lattice. Replacing by and using evenness changes this difference to its negative, so and . Hence is doubly periodic.
It therefore descends to a meromorphic function on , with a double pole at zero modulo the lattice and no others. A meromorphic function is a holomorphic map to the Riemann sphere, sending poles to infinity. Locally at zero, is holomorphic and vanishes there, so the sphere chart at infinity supplies the required extension. The map is nonconstant because it has a pole.
The total pole order in one period cell is two, so the map has degree two. The Riemann-Hurwitz formula for genus one to genus zero gives , hence . Each local degree is at most two, so every ramification contribution is exactly one. Therefore
They are zero and the three nonzero half-period classes. Zero is ramified because its reciprocal has a double zero. At a nonzero half-period, oddness and periodicity of force ; the count shows these exhaust the remaining points.
For a degree-two map to the Riemann sphere, the Riemann-Hurwitz formula gives . Again each ramification index is two, so the number of ramification points equals . Thus
For a regular parametrization , the first fundamental form is the induced metric
It measures the lengths and angles of tangent vectors. A geodesic is a curve whose unit tangent has zero covariant derivative along itself. For an arc-length parametrized surface curve in Euclidean three-space, this means its acceleration is normal to the surface, or .
Since , we have . The normal-acceleration characterization of a geodesic gives
Expanding and differentiating the metric coefficients yields , , and . Therefore
Applying the same calculation to gives
These are also the Euler-Lagrange equations of the quadratic metric energy.
For the surface of revolution, the arc-length condition on its profile gives , , . Thus the geodesic equations reduce to
Consequently
the Clairaut first integral for a surface of revolution.
On a meridian, take and . Both equations hold, so every meridian is a geodesic. On a cross-section , arc length requires . The first equation then holds exactly when , while the second holds automatically. Hence

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