2023MNRAS.526L..20H

Gravity is the driving force of star formation. Although gravity is caused by the presence of matter, its role in complex regions is still unsettled. One effective way to study the pattern of gravity is to compute the accretion it exerts on the gas by providing gravitational acceleration maps. A practical way to study acceleration is by computing it using 2D surface density maps, yet whether these maps are accurate remains uncertain. Using numerical simulations, we confirm that the accuracy of the acceleration maps a_2D(x, y) computed from 2D surface density are good representations for the mean acceleration weighted by mass. Due to the underestimations of the distances from projected maps, the magnitudes of accelerations will be overestimated $|\mathbf {a}_{\rm 2D}(x,y)| \approx 2.3 \pm 1.8 \,\, |\mathbf {a}_{\rm 3D}^{\rm proj}(x,y)|$, where $\mathbf {a}_{\rm 3D}^{\rm proj}(x,y)$ is mass-weighted projected gravitational acceleration, yet a_2D(x, y) and $\mathbf {a}_{\rm 3D}^{\rm proj}(x,y)$ stay aligned within 20°. Significant deviations only occur in regions where multiple structures are present along the line of sight. The acceleration maps estimated from surface density provide good descriptions of the projection of 3D acceleration fields. We expect this technique useful in establishing the link between cloud morphology and star formation, and in understanding the link between gravity and other processes such as the magnetic field. A version of the code for calculating surface density gravitational potential is available at https://github.com/zhenzhen-research/phi_2d.