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Borsuk–Ulam theorem

Statement

For every continuous map f:Sn→Rnf: S^n \to \mathbb{R}^n there is a point x∈Snx \in S^n with f(x)=f(−x)f(x) = f(-x). Equivalently, there is no continuous map Sn→Sn−1S^n \to S^{n-1} satisfying f(−x)=−f(x)f(-x) = -f(x) for every xx.

Why is it true?

At every moment, there exist two antipodal points on Earth's surface (opposite ends of a diameter through the centre) with exactly the same temperature and exactly the same barometric pressure simultaneously, because temperature and pressure vary continuously and n=2n=2 here.

Proof sketch

The theorem can be derived from a covering lemma of Lusternik and Schnirelmann: if SnS^n is covered by n+1n+1 closed sets, at least one of them must contain a pair of antipodal points. Applying this to sets built from ff (partitioning SnS^n according to which coordinate of f(x)f(x) is largest in absolute value) forces f(x)=f(−x)f(x)=f(-x) for some xx; the theorem can also be proved directly via a degree/index argument on the map g(x)=f(x)−f(−x)g(x)=f(x)-f(-x).

Topics that use this theorem

Related theorems

Step-by-step proofs

No step-by-step proof yet for this theorem.

References

  1. Karol Borsuk (1933). Drei Sätze über die n-dimensionale euklidische Sphäre
  2. Jiří Matoušek (2003). Using the Borsuk–Ulam Theorem