Shadow-Induced Warps in Protoplanetary disks
Shangjia Zhang, Zhaohuan Zhu, Callum W. Fairbairn
TL;DR
This work shows that shadows cast by a misaligned inner disk can thermally drive global warps in outer protoplanetary disks, with a 30° inclination producing stronger accretion and a pronounced outer warp (tilt up to ~$32^{\circ}$ relative to the inner disk) than polar configurations. Using 3D radiation–hydrodynamical simulations and pure hydro runs with prescribed temperature structures, the authors demonstrate that the warp is driven by an $m=1,n=1$ temperature perturbation, whose influence peaks near a mutual inclination of ~$15^{\circ}$ but remains significant from $3^{\circ}$ to $30^{\circ}$. They establish a semi-quantitative scaling between the $m=1,n=1$ mode amplitude and disk tilt, show that an outer exponential cutoff enhances inter-disk twisting, and reveal periodic tilt oscillations with periods of order $10^2$–$10^3$ years in full-disk models. The findings offer concrete, testable predictions for ALMA and NIR observations, enabling forward modeling of shadow-induced dynamics by directly constraining the azimuthal–vertical temperature structure and comparing it to the disk’s density and velocity responses.
Abstract
Shadows are commonly observed in protoplanetary disks in near-infrared and (sub)millimeter images, often cast by misaligned inner disks or other obscuring material. While recent studies show that shadows can alter disk dynamics, only the case symmetric across the midplane (e.g., from a polar-aligned inner disk) has been studied. Here we study shadows cast by an inner disk with a $30^\circ$ mutual inclination using 3D radiation-hydrodynamical simulations. Given the same shadow shape and amplitude, the $30^\circ$ inclined shadow leads to a much stronger accretion compared with the polar case, reaching $α\sim$ 1, because the disk is squeezed twice in one azimuth, leading to shocks and strong radial flows near the midplane. The outer disk develops a warp: the inner disk region tilts toward alignment with the shadow, while the outer, exponentially tapered disk tilts and twists in a different direction, inclined $\sim$ 32$^\circ$ relative to the inner region. Locally isothermal simulations with a prescribed temperature structure reproduce the effect, confirming that it is thermally driven. Fourier-Hermite analysis shows that it is the m=1, n=1 temperature perturbation that drives the warp by launching bending waves, with the tilting response of the disk approximately proportional to the modal amplitude. This mode always exists unless the shadow is coplanar or polar. Given a fixed temperature contrast, the m=1,n=1 mode peaks at $\sim$15$^\circ$ mutual inclination, but still contributes substantially across 3$^\circ$ to 30$^\circ$. Shadows cause disk warps--they are not only a consequence of them. We discuss testable predictions for current and future ALMA and NIR observations.
