North and south magnetic poles are not that simple to find. There are two solutions to the vector magnetostatics equilibrium problem of the Earth. The first one has the north and south magnetic poles right at the top of the magnetosphere, and the other one has the poles in the middle of the Earth.
This controversy has been known since the 1920s and the question is still open. What's obvious is that although the magnetic field can be perfectly dipolar, the magnetic pole and geomagnetic pole are far from being coincident. The difference between the two is not very large, but they are not equal.
The geomagnetic pole differs from the magnetic dipole in two main ways. First, the dipole is a single point, but the pole has a finite width. The dipole is the complete magnetic field, the pole has a finite width but no endpoints.
The second difference is that the dipole is a line, but the pole is a circle. This means that the dipole is a topological feature, but the pole is a geometrical feature. The magnetic and geomagnetic field can have the same topology, but they will diverge in the directions perpendicular to the direction of the field.
This is because the field from the dipole, the magnetic dipole, can be added up to a point or to a line. If you add the field from the dipole to a point, the result is a sphere. If you add the field from the dipole to a line, the result is a cylinder. If you add the field from the dipole to both a line and a point, the result is a cone. So it may seem a natural choice to place the poles where a torus can be formed by connecting a line and a point with a cylinder.
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