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Geodesics in the Poincare upper half-plane

Example

For the Poincaré metric g=(dx2+dy2)/y2 on H={(x,y)R2:y>0}, every nonconstant affinely parametrized geodesic is a restriction of exactly one of the following forms, with k0: γ(t)=(a,bekt)(aR, b>0), γ(t)=(a+Rtanh(kt+c), Rsech(kt+c))(a,cR, R>0). Conversely, each displayed curve on all of R is a geodesic and traces a whole vertical line or upper Euclidean semicircle (xa)2+y2=R2 orthogonal to the boundary y=0; a restriction traces the corresponding subarc. Constant curves are the zero-speed geodesics. An affine change of parameter merely changes the constants in these displayed parametrizations.

Facts & Assumptions

Given: The upper half-plane H, its displayed metric, and a geodesic on an interval I.

[F1]

Christoffel formula for the levi civita connection computes Levi–Civita symbols from the metric matrix; Coordinate geodesic equation makes the coordinate ODE equivalent to the intrinsic geodesic condition.

[F3]

The natural logarithm has derivative 1/x and equals the integral from 1 to x of 1/t gives (logy)=1/y for y>0, and The natural logarithm as the inverse of the exponential function makes log the inverse of exp on positive reals.

[F4]

The functions tanh and sech are defined on all of R by The six hyperbolic functions and their natural domains; Addition formulas, identities, parity, and derivatives of the hyperbolic functions gives tanh=sech2, sech=sechtanh, tanh2+sech2=1, and the range tanh(R)=(1,1).

[F6]

The exponential addition formula exp(x+y)=exp(x)exp(y) gives exp(u+v)=exp(u)exp(v).

Verification

1.1

Here (gij)=y2I2 and (gij)=y2I2. Applying the formula in [F1], the only nonzero symbols are Γxxy=Γxyx=1/y, Γyxx=1/y, and Γyyy=1/y. Hence the two geodesic equations are x2xy/y=0,y+(x2y2)/y=0.

F1given
2.1

The first equation gives (x/y2)=0, so C:=x/y2 is constant by [F2]. Differentiating E:=(x2+y2)/y2 gives E=2xy2(x2xy/y)+2yy2(y+(x2y2)/y)=0. Thus E is constant too. If E=0, positive definiteness forces x=y=0, and the curve is constant.

F2F7step 1.1given
3.1

If C=0, then x=0, so x=a. The second equation becomes (logy)=(yyy2)/y2=0. By [F2], [F3] and [F7], logy=kt+d; therefore [F6] gives y=bekt with b=ed>0. A nonconstant curve has k0. Conversely, [F5] and [F7] give x=0 and y=y2/y for x=a, y=bekt, so both equations in step 1.1 hold.

F2F3F5F6F7step 1.1step 2.1
3.2

Suppose C0. Put a:=x+y/(Cy). From the second equation and x=Cy2, a=x+(yyy2)/(Cy2)=Cy2x2/(Cy2)=0. Thus a is constant. Since E>0, set R=E/C>0. Direct substitution into the identity defining E gives (xa)2+y2=E/C2=R2. In particular z:=(xa)/R lies in (1,1), and y=R1z2.

F2F7step 1.1step 2.1
4.1

Define u=12log((1+z)/(1z)), which is defined because z<1. The logarithm, chain and quotient rules give u=z/(1z2), while z=x/R=Cy2/R=CR(1z2); hence u=CR=:k0. By [F2], u=kt+c. The inverse-log law in [F3] and exponential addition [F6] give e2u=(1+z)/(1z), so the definitions in [F4] give z=tanhu; since y>0 and 1tanh2u=sech2u, y=Rsechu. This yields the stated semicircle parametrization on the entire interval.

F2F3F4F6F7step 2.1step 3.2
5.1

Conversely, set U=kt+c, T=tanhU, and S=sechU. For x=a+RT and y=RS>0, [F4] and [F7] give x=RkS2, y=RkST, x=2Rk2S2T, and y=Rk2S(2T21). The first equation of step 1.1 has left side 2Rk2S2T+2Rk2S2T=0; the second has left side Rk2S(T2+S21)=0. These curves therefore are geodesics. The identity (xa)2+y2=R2 shows the circle meets y=0 at right angles; S>0 and the range of tanh show the whole upper semicircle is traced as t ranges over R.

F1F4F7step 1.1step 4.1
6.1

The alternatives E=0, C=0<E, and C0 exhaust every geodesic. In the vertical case the curve determines a=x, k=(logy), d=logykt and b=ed. In the semicircle case its invariants determine a=x+y/(Cy), R=E/C, k=CR, u=12log((1+z)/(1z)) and c=ukt. Hence, for the fixed affine parameter, the displayed constants are unique. Steps 3.1 and 5.1 verify both nonconstant families, including their restrictions to intervals with endpoints. For an affine parameter change tαt+β with α0, the first family changes b,k and the second changes k,c; α=0 yields a constant curve. No countable choice or geodesic existence theorem is used: the conclusion follows by integrating the given curve's own ODE.

F3step 2.1step 3.1step 3.2step 4.1step 5.1

Source locator

Datar, Example 15.1.6, p. 115, supplies the metric and coordinate geodesic equations. Its final printed circle equation has the coordinate roles of the center interchanged; the boundary-centered equation used here follows from the calculation in step 3.2.

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Sources