Updated Kinematics of the Radcliffe Wave: Nonsynchronous, Dipole-like Vertical Oscillations

Data de publicació

2025-05-19T09:56:13Z

2025-05-19T09:56:13Z

2024

2025-05-19T09:56:13Z

Resum

The kinematic information of the Radcliffe wave (RW) is essential for determining its existence and gaining insights into its origin and evolution. In this work, we present an accurate measurement of the vertical velocity (VZ) of the RW by incorporating the radial velocity (RV) measures through two methods, which is crucial but was neglected previously. First, the velocities are measured toward young stars, using their RV measurements from APOGEE-2 and proper motion measurements from Gaia DR3. Second, we combine RV measurements toward clouds with proper motion measurements of associated young stellar objects to determine the vertical velocities of the clouds. The results reveal that the oscillations in VZ are not synchronous with the vertical coordinate Z, which differs from the conclusions of previous studies. Instead, we find a 5 km s−1 kpc−1 gradient in VZ along the RW, exhibiting a dipole-like pattern. Consequently, the kinematic arrangement does not show a corresponding coherence with the spatial arrangement, bringing the RW model into question.

Tipus de document

Article


Versió publicada

Llengua

Anglès

Publicat per

Institute of Physics (IOP)

Documents relacionats

Reproducció del document publicat a: https://doi.org/10.3847/1538-4357/ad66cd

Astrophysical Journal, 2024, vol. 971, num.167

https://doi.org/10.3847/1538-4357/ad66cd

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(c) American Astronomical Society, 2024

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