Abstract

Realizing the no-boundary proposal of Hartle and Hawking as a consistent gravitational path integral has been a long-standing puzzle. In particular, it was demonstrated by Feldbrugge, Lehners, and Turok that the sum over all universes starting from a zero size results in an unstable saddle point geometry. Here we show that, in the context of gravity with a positive cosmological constant, path integrals with a specific family of Robin boundary conditions overcome this problem. These path integrals are manifestly convergent and are approximated by stable Hartle-Hawking saddle point geometries. The price to pay is that the off-shell geometries do not start at a zero size. The Robin boundary conditions may be interpreted as an initial state with Euclidean momentum, with the quantum uncertainty shared between the initial size and momentum.

Highlights

  • If the quantum theory is universal, and there currently is no reason to think otherwise, the Universe should be describable by a quantum state just like any other system

  • In this Letter, we will combine several of the ideas mentioned above, using Robin boundary conditions in order to impose a condition on a linear combination of the initial size and momentum of the Universe

  • For a family of such conditions, we find that the path integral can be approximated solely by the stable no-boundary saddle points, avoiding instabilities and representing a consistent definition of the no-boundary proposal

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Summary

Published by the American Physical Society

H2qÞ : The integration domain for the lapse is N ∈ ð0þ; ∞Þ, ensuring that the geometries in the sum have a Lorentzian signature This makes the path integral a propagator in the sense that it solves the inhomogeneous Wheeler-DeWitt equation H G1⁄2q1; 0Š 1⁄4 −iδðq1Þ, where His the quantum Hamiltonian. That the integral along the positive real N line is equivalent to the integral along the steepest descent path (“thimble”) running through this saddle point alone; see Fig. 1. There is, no convergent contour which can be deformed into a steepest descent path running through solely these two saddle points [6] In this sense, the wave function (3) is not the saddle point approximation of the no-boundary wave function for any Lorentzian path integral with these boundary conditions. Let us consider augmenting the action with a Robin boundary term at the initial surface: Stot

The variation of the full action is now δStot
Nt þ
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