Carleson's theorem
Statement
For every square-integrable periodic function , the symmetric partial sums of its Fourier series, where , converge pointwise to as for Lebesgue-almost every . (Extended by Richard Hunt in 1968 to every with .)
Why is it true?
Parseval's identity guarantees that the Fourier partial sums converge to in average energy, so Nikolai Luzin conjectured in 1915 that should also converge at almost every individual point . Yet Andrey Kolmogorov shocked analysts in 1923–1926 by constructing an integrable function whose Fourier series diverges everywhere, making many suspect Luzin's conjecture was false even for . Lennart Carleson proved in 1966 that finite energy is strong enough to tame the wild oscillations of the Dirichlet kernel: destructive interference across scales prevents the partial sums from blowing up except on a set of measure zero.
Proof sketch
Because trigonometric polynomials are dense in and converge pointwise everywhere, Stein's maximal principle reduces almost-everywhere convergence to proving a weak-type bound for the Carleson maximal operator , namely . Expressing via the Dirichlet kernel shows is controlled by , a modulated singular integral. Carleson decomposed the time-frequency plane into dyadic rectangles (tiles) and combinatorially organized them into trees to bound the interactions across both space and frequency; in 2000, Michael Lacey and Christoph Thiele gave a streamlined time-frequency phase-plane proof.
Topics that use this theorem
Related theorems
Step-by-step proofs
No step-by-step proof yet for this theorem.
References
- Lennart Carleson (1966). On convergence and growth of partial sums of Fourier series · DOI:10.1007/BF02392815
- Michael Lacey, Christoph Thiele (2000). A proof of boundedness of the Carleson operator · DOI:10.4310/MRL.2000.v7.n4.a1