Reconstructing the Sun's Alfvén surface and wind braking torque with Parker Solar Probe
Adam J. Finley
TL;DR
This study reconstructs the Sun's Alfvén surface, $r_A$, using Parker Solar Probe measurements during solar cycle 25, linking in-situ solar wind data with coronal magnetic-field structure via Parker spiral physics and PFSS modelling. The Alfvén radius grows from ~11 to ~16 $R_\odot$ as activity increases, with fluctuations of 10–40% over both space and time; the corresponding solar wind angular momentum-loss rate rises from ~1×10^{30} erg to ~3×10^{30} erg, following the cycle. The results show that $r_A$ scales with wind magnetisation $\Upsilon_{\text{open}}$, but PSP measurements yield ~30% larger radii than 2.5D wind simulations for the same $\dot{M}$ and $\phi_{\text{open}}$, suggesting missing physics such as 3D geometry, time variability, or turbulence. The work highlights the complex, corrugated Alfvén surface shaped by coronal field evolution and underscores the value of combining in-situ measurements with global coronal models to test angular-momentum loss in Sun-like stars. Future missions extending measurements in latitude and remote sensing will further constrain the large-scale Alfvén-surface morphology and its role in stellar spin-down.
Abstract
The Alfvén surface -- where the solar wind exceeds the local Alfvén speed as it expands into interplanetary space -- is now routinely probed by NASA's Parker Solar Probe (PSP) in the near-Sun environment. The size of the Alfvén surface governs how efficiently the solar wind braking torque causes the Sun to spin-down. We aimed to characterise the size and evolution of the Alfvén surface as magnetic activity increased during solar cycle 25. The Alfvén surface was extrapolated from the solar wind mass and magnetic flux measured by the SWEAP and FIELDS instrument suites onboard PSP. We accounted for the acceleration of the solar wind along Parker spiral magnetic field lines and used potential field source surface modelling to determine the sources of the solar wind. The longitudinally averaged Alfvén radius measured by PSP grew from 11 to 16 solar radii as solar activity increased. Accordingly, the solar wind angular momentum-loss rate grew from $\sim$1.4$\times 10^{30}$ erg to 3$\times 10^{30}$ erg. Both the radial and longitudinal scans of the solar wind contained fluctuations of 10-40\% from the average Alfvén radius in each encounter. Structure in the solar corona influenced the morphology of the Alfvén surface, which was smallest around the heliospheric current sheet and pseudostreamers. The Alfvén surface was highly structured and time-varying however, at large-scales, organised by the coronal magnetic field. The evolution of the solar corona over the solar cycle systematically shifted the magnetic connectivity of PSP and influenced our perception of the Alfvén surface. The Alfvén surface was 30\% larger than both thermally-driven and Alfvén wave-driven wind simulations with the same mass-loss rate and open magnetic flux, but had a similar dependence on the wind magnetisation parameter.
