2025MNRAS.539..820L

The classical Laplace surface defines the location of circular particle orbits that do not undergo nodal precession around a planet with some obliquity. Close to the planet the surface coincides with the equator of the planet, while far from the planet it coincides with the orbital plane of the planet. We determine the shape of the Laplace surface of a circumplanetary disc that results from accretion of circumstellar gas and experiences the effects of gas pressure, self-gravity, and viscosity, as well as the gravitational effects due to the planetary spin and the star. We apply the linear theory of warped discs in the wave-like regime for a small-obliquity planet such as Jupiter. As a result of dissipation, a disc that begins slightly away from its Laplace surface will evolve to it. Because of pressure effects in typically warm circumplanetary discs, the disc is highly flattened compared with the classical Laplace surface, meaning that it is much less warped but still significantly tilted. For the case of Jupiter, the disc does not align anywhere with the equator of the planet. For such discs, the effects of self-gravity and viscosity on warping are typically small. The disc tilt is intermediate between the planet's equatorial and orbital planes. Circumplanetary discs that are much cooler than expected can undergo warping and alignment with the planet's equator at small radii. The results have implications for the orbital evolution of satellites in the Solar system that are observed to be somewhat aligned with their classical Laplace surface.