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TauCeti.NumberTheory.ModularForms.GeodesicIntegral.BetweenCusps

Integrals along geodesics between cusps, and their additivity #

For F : ℍ → ℂ and cusps a, b ∈ ℙ¹(ℚ), this file defines the integral TauCeti.cuspIntegral F a b = ∫_a^b F(z) dz of the one-form F(z) dz along the hyperbolic geodesic from a to b: it is the geodesic integral g.geodesicIntegral F of TauCeti.NumberTheory.ModularForms.GeodesicIntegral.Basic for any rational matrix g of positive determinant with g • 0 = a and g • ∞ = b, which only depends on the endpoints.

The main result is additivity, ∫_a^b F(z) dz + ∫_b^c F(z) dz = ∫_a^c F(z) dz: Cauchy's theorem for the ideal triangle with vertices a, b, c, all three of which lie on the boundary. It holds for holomorphic F whose weight-2 slashes F ∣[2] g by rational matrices of positive determinant are integrable near i∞ along the imaginary axis and tend to 0 at i∞ uniformly on vertical strips; the period integrand f(z) P(z, 1) of a cusp form satisfies both conditions (TauCeti.NumberTheory.ModularForms.ModularSymbols.Period.Integral). The proof uses a primitive Φ of F on ℍ (TauCeti.Analysis.Complex.UpperHalfPlane.Primitive), whose composite with g is a primitive of F ∣[2] g. The first condition gives Φ a limit at each cusp along each geodesic ending there; the second shows that the limit at a cusp does not depend on the geodesic, since after moving the cusp to i∞ two such geodesics become vertical lines, joined by horizontal segments on which F ∣[2] g is uniformly small. Each geodesic integral is then the difference of the values of Φ at its endpoints, and additivity follows.

Additivity is what makes the periods of a cusp form a function of degree-zero divisors on the cusps, the first step of the period pairing between cusp forms and modular symbols.

The same primitive also computes integrals from a point τ ∈ ℍ to i∞ along the vertical ray z = τ + i t, as its limit at i∞ minus its value at τ. Comparing this with its values at the cusps gives the substitution z ↦ g • z in such an integral: the image of the vertical ray from τ ends at the cusp g • ∞, and is replaced by the vertical ray from g • τ followed by the geodesic from i∞ to g • ∞. This is how the Eichler integral ∫_τ^{i∞} f(z) (z - τ)ⁿ dz of a cusp form transforms under SL(2, ℤ) up to periods.

Main definitions #

Main results #

References #

Primitives on the upper half-plane #

Limits of a primitive at i∞ #

Values of a primitive at the cusps #

Integrals between cusps #

noncomputable def TauCeti.cuspIntegral (F : UpperHalfPlane → ℂ) (a b : OnePoint ℚ) :

The integral ∫_a^b F(z) dz of the one-form F(z) dz along the hyperbolic geodesic from the cusp a to the cusp b of ℙ¹(ℚ). For a ≠ b it is g.geodesicIntegral F for any rational matrix g of positive determinant with g • 0 = a and g • ∞ = b, the choice not mattering (cuspIntegral_smul_zero_smul_infty); for a = b it is 0. Both endpoints are improper, and, as for Matrix.GeneralLinearGroup.geodesicIntegral, the value is 0 when the integrand is not integrable.

Equations
Instances For

    The integral between the cusps g • 0 and g • ∞ is the geodesic integral along g.

    @[simp]

    The integral from a cusp to itself vanishes.

    Reversing the orientation changes the sign: ∫_b^a F(z) dz = -∫_a^b F(z) dz.

    theorem TauCeti.cuspIntegral_slash (F : UpperHalfPlane → ℂ) {γ : GL (Fin 2) ℚ} (hγ : 0 < (↑γ).det) (a b : OnePoint ℚ) :
    cuspIntegral (SlashAction.map 2 γ F) a b = cuspIntegral F (γ • a) (γ • b)

    The substitution z ↦ γ • z: for γ of positive determinant, the integral of the pulled-back one-form (F ∣[2] γ)(z) dz from a to b is the integral of F(z) dz from γ • a to γ • b.

    theorem TauCeti.cuspIntegral_smul (c : ℂ) (F : UpperHalfPlane → ℂ) (a b : OnePoint ℚ) :
    cuspIntegral (c • F) a b = c * cuspIntegral F a b

    The integral between cusps is homogeneous under scalar multiplication of the integrand: ∫_a^b c F(z) dz = c ∫_a^b F(z) dz. Additivity in the integrand needs integrability, and holds under the hypotheses of TauCeti.cuspIntegral_add.

    @[simp]

    The integral of the zero integrand between two cusps vanishes.

    The integral between the cusps g • 0 and g • ∞ is additive in the integrand when both integrands are integrable along the geodesic g.

    theorem TauCeti.cuspIntegral_sum {ι : Type u_1} (s : Finset ι) {F : ι → UpperHalfPlane → ℂ} {g : GL (Fin 2) ℚ} (hg : 0 < (↑g).det) (hF : ∀ i ∈ s, MeasureTheory.IntegrableOn (UpperHalfPlane.resToImagAxis (SlashAction.map 2 g (F i))) (Set.Ioi 0) MeasureTheory.volume) :
    cuspIntegral (∑ i ∈ s, F i) (g • ↑0) (g • OnePoint.infty) = ∑ i ∈ s, cuspIntegral (F i) (g • ↑0) (g • OnePoint.infty)

    The integral between the cusps g • 0 and g • ∞ commutes with finite sums of integrands that are integrable along the geodesic g.

    theorem TauCeti.cuspIntegral_add_adjacent {F : UpperHalfPlane → ℂ} (hF : MDiff F) (hint : ∀ (g : GL (Fin 2) ℚ), 0 < (↑g).det → MeasureTheory.IntegrableOn (UpperHalfPlane.resToImagAxis (SlashAction.map 2 g F)) (Set.Ici 1) MeasureTheory.volume) (hdecay : ∀ (g : GL (Fin 2) ℚ), 0 < (↑g).det → ∀ (a b : ℝ), Filter.Tendsto (SlashAction.map 2 g F) (UpperHalfPlane.atImInfty ⊓ Filter.principal {τ : UpperHalfPlane | τ.re ∈ Set.Icc a b}) (nhds 0)) (a b c : OnePoint ℚ) :

    Additivity of integrals between cusps: ∫_a^b F(z) dz + ∫_b^c F(z) dz = ∫_a^c F(z) dz for a holomorphic F whose weight-2 slashes by rational matrices of positive determinant are integrable near i∞ along the imaginary axis and tend to 0 at i∞ uniformly on vertical strips. These are the conditions under which the integrals along the three sides of the ideal triangle with vertices a, b, c are computed by a primitive Φ of F: each is the difference of the limits of Φ at its two endpoints, and the limit of Φ at a cusp does not depend on the geodesic along which the cusp is approached.

    Integrals from a point of ℍ to i∞ #

    The substitution z ↦ g • z in an integral from a point of ℍ to i∞. For g a rational matrix of positive determinant and τ ∈ ℍ,

    ∫_τ^{i∞} (F ∣[2] g)(z) dz = ∫_{g • τ}^{i∞} F(z) dz + ∫_{i∞}^{g • ∞} F(z) dz,

    the integrals from τ and from g • τ taken along the vertical rays z = τ + i t and z = g • τ + i t, t > 0, and the last along the geodesic between the two cusps. The left side is the integral of F(z) dz along the image under g of the vertical ray from τ, which ends at the cusp g • ∞, and the identity is Cauchy's theorem for the triangle with vertices g • τ, g • ∞ and i∞. The hypotheses on F are those of TauCeti.cuspIntegral_add_adjacent, and the two vertical integrands are assumed integrable.