End of the world brane in double scaled SYK
Kazumi Okuyama
TL;DR
This work analyzes the end-of-the-world (EOW) brane in the double-scaled SYK (DSSYK) model, showing the boundary state is a coherent state of $q$-deformed oscillators and the EOW wavefunction is described by the continuous big $q$-Hermite polynomial. In a triple scaling limit, this wavefunction reproduces the JT gravity Whittaker function, establishing a concrete bridge between DSSYK and JT gravity with EOW branes. The half-wormhole amplitude in DSSYK factorizes into a trumpet component and a brane-dependent factor, mirroring the JT result and providing a precise holographic interpretation of EOW brane effects in the DSSYK ensemble. The findings reveal quantized bulk lengths controlled by the DSSYK parameter $\\lambda$, and suggest avenues for generalizations to multiple branes and matter couplings, offering a pathway toward a richer DSSYK-based gravity dictionary.
Abstract
We study the end of the world (EOW) brane in double scaled SYK (DSSYK) model. We find that the boundary state of EOW brane is a coherent state of the $q$-deformed oscillators and the associated orthogonal polynomial is the continuous big $q$-Hermite polynomial. In a certain scaling limit, the big $q$-Hermite polynomial reduces to the Whittaker function, which reproduces the wavefunction of JT gravity with an EOW brane. We also compute the half-wormhole amplitude in DSSYK and show that the amplitude is decomposed into the trumpet and the factor coming from the EOW brane.
