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The Riemann sphere

The unit sphere sits in the complex plane, meeting it along the equator, which is therefore the plane's own unit circle. Joining a point z of the plane to one pole of the sphere by a straight line marks a second point P where that line crosses the sphere: this correspondence is stereographic projection. The pole one projects from answers to z = ∞, and the opposite pole to z = 0, so that the sphere is the plane with a single point at infinity added — the Riemann sphere.

Project from

What to look for

Three collinear points. Pick a point z on the plane, join it to the south pole marked ; the line ray ∞z meets the sphere again at P, called the stereographic projection of z. The three points are collinear by construction. Notice that when z lies inside the unit circle, its stereographic projection P is on the upper hemisphere; when z lies outside the unit circle, its stereographic projection P is on the lower hemisphere .

Where the poles go. Drag z toward the origin and P climbs to the pole marked 0; push z far away in any direction and P settles toward the pole marked , from whichever side it approached. Every direction of escape in the plane arrives at the same point of the sphere: the plane has many ways to run off to infinity, and the sphere collapses them all into one point. That single added point is what makes the sphere compact — and what makes it the natural home of the plane.

The equator is not drawn. Look where the sphere meets the plane. No equator has been drawn anywhere: the curve you see is simply the plane's own unit circle, which is where the two surfaces cross. And the unit circle is exactly the set that the projection leaves alone — put z on it and P lands on top of z, for either choice of pole.

Angles survive; areas do not. The projection is conformal: it preserves angles everywhere. Switch on the figure and drag it about — its corners keep their angles wherever it goes, while its size does not: the local magnification is λ = 2/(1 + |z|²), reported in the panel. It is largest at the origin and dies away toward infinity, so the neighbourhood of the pole marked is smeared over the whole far reach of the plane.

Which pole to project from. That last fact settles a cartographic question. Whichever pole we project from is the one whose neighbourhood gets stretched beyond recognition, so we project from the pole we care least about. For a map of the Earth that is the south pole, and this lesson projects from the south by default; the Antarctic is what gets banished to the edge. There is a second reason, harder to see and just as real: projected from the south, a figure and its image on the sphere have the same handedness — switch the pole to the north and watch the flag's pennant change sides.