The q-coordinate of a normalized cusp datum #
For a cusp datum with scaling σ and width w, the coordinate is
q(z) = exp (2 * π * I * σ(z) / w). Its fibres are exactly the orbits of the full cusp
stabilizer. It therefore identifies the stabilizer quotient of the upper half-plane with the
punctured unit disc. The forward map is the q-coordinate and the inverse is the orbit of a
logarithmic lift transported back by σ⁻¹.
This uses the translation quotient computed in
TauCeti.Analysis.Complex.UpperHalfPlane.CuspCoordinate. No discreteness assumption is needed
once a normalized cusp datum is given: its primitive-generator condition identifies the full
stabilizer. The coordinate is holomorphic, and scaled horodiscs of positive height correspond
exactly to smaller punctured discs. This is a local model for cusp charts; embedding such a
neighbourhood into the full group quotient additionally requires precise invariance of the horodisc.
References #
- Fred Diamond and Jerry Shurman, A First Course in Modular Forms, §2.4.
- Otto Forster, Lectures on Riemann Surfaces, §19.
The exponential coordinate of a normalized cusp datum on the upper half-plane.
Equations
Instances For
The cusp coordinate is the q-parameter of the scaled point, with the datum's width.
Applying the inverse scaling before the cusp coordinate recovers the ordinary q-parameter.
The exponential cusp coordinate never vanishes on the upper half-plane.
The exponential cusp coordinate lies in the open unit disc.
In scaling coordinates, the selected generator acts by translation through the width.
The exponential cusp coordinate is invariant under the full cusp stabilizer.
Continuous lifts with the same q-projection agree if they agree at one point of a preconnected source.
In the scaling coordinate, powers of the primitive cusp generator are integral-width translations.
The exponential coordinate, regarded as a map into the punctured unit disc.
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Evaluation of the normalized q-coordinate as the width parameter after scaling.
The normalized q-coordinate is the width parameter composed with scaling.
The q-coordinate has exactly the full cusp-stabilizer orbits as its fibres.
Two points have the same q-coordinate exactly when they differ by an integer power of the selected generator.
The q-coordinate is invariant under the full stabilizer, not just the selected generator.
The q-coordinate is invariant under any group element fixing the cusp.
The scaled logarithmic lift is a right inverse of the q-coordinate.
The q-coordinate identifies the quotient by the full cusp stabilizer with the punctured unit disc.
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The quotient homeomorphism sends the orbit of a point to its q-coordinate.
The inverse quotient homeomorphism sends a punctured-disc point to the orbit of its width-dependent logarithmic lift transported back by the inverse scaling.
The normalized q-coordinate is an open quotient map.
The normalized q-coordinate is holomorphic as a map into the punctured unit disc.
The normalized q-coordinate, regarded as a complex-valued function, is holomorphic.
A scaled horodisc is exactly the inverse image of a punctured disc under the q-coordinate.
The image of a scaled horodisc is the punctured disc of the corresponding exponential radius.
The q-coordinate tends to zero whenever the height in the scaling coordinate tends to infinity. The limit is through nonzero values, as required for a punctured cusp chart.