(D. Ruffolo*, N. Ngampoopun, Y. R. Bhora, P. Thepthong, P. Pongkitiwanichakul, W. H. Matthaeus, and R. Chhiber, Astrophys. J., 923, 158)
This work was motivated by our previous work that proposed that an instability between solar wind streams in interplanetary space with different velocities can explain an observed transition in solar wind fluctuations, can strongly energize turbulence in the solar wind, and can explain “switchbacks” or temporary reversals in the interplanetary magnetic field (Ruffolo et al. 2020; see https://physics.sc.mahidol.ac.th/research/highlights/Ruffolo-2021-a/). That work commented on domains of nearly constant magnetic pressure in the solar wind. Actually the velocity V and magnetic field B of solar wind plasma undergo very strong turbulent fluctuations, but often these are so-called Alfvénic fluctuations that nearly conserve the magnetic field magnitude |B| and the magnetic pressure (which is proportional to |B|2).
Here we examined domains of approximate magnetic pressure balance in detail, using public data from NASA’s Parker Solar Probe (PSP), mankind’s first spacecraft to travel close to the Sun, for the first 5 orbits. We analyzed data from the FIELDS and SWEAP instrument suites. We developed a systematic definition of contiguous domains, as illustrated in Figure 1. We found that the mean domain duration generally has an inverse relationship with plasma β (ratio of plasma pressure to magnetic pressure) and is otherwise not dependent on distance from the Sun, and domains have an aspect ratio consistent with a spherical (isotropic) shape.