4.7 Article

The Radial Evolution of the Solar Wind as Organized by Electron Distribution Parameters

Journal

ASTROPHYSICAL JOURNAL
Volume 936, Issue 1, Pages -

Publisher

IOP Publishing Ltd
DOI: 10.3847/1538-4357/ac85b8

Keywords

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Funding

  1. SWEAP team [NNN06AA01C]
  2. PSP mission
  3. LWS management

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We used observations from the Parker Solar Probe to study the radial evolution of solar wind in the inner heliosphere. Our analysis showed that the electron temperature and electric potential are negatively correlated with wind speed, indicating that the electron thermal pressure and electric field accelerate the slow wind more than the fast wind. Furthermore, we found that both electric field driven exospheric models and thermally driven hydrodynamic models can explain the observed speed of the slowest solar wind streams, but additional acceleration mechanisms are required to explain the faster streams.
We utilize observations from the Parker Solar Probe (PSP) to study the radial evolution of the solar wind in the inner heliosphere. We analyze electron velocity distribution functions observed by the Solar Wind Electrons, Alphas, and Protons suite to estimate the coronal electron temperature and the local electric potential in the solar wind. From the latter value and the local flow speed, we compute the asymptotic solar wind speed. We group the PSP observations by asymptotic speed, and characterize the radial evolution of the wind speed, electron temperature, and electric potential within each group. In agreement with previous work, we find that the electron temperature (both local and coronal) and the electric potential are anticorrelated with wind speed. This implies that the electron thermal pressure and the associated electric field can provide more net acceleration in the slow wind than in the fast wind. We then utilize the inferred coronal temperature and the extrapolated electric + gravitational potential to show that both electric field driven exospheric models and the equivalent thermally driven hydrodynamic models can explain the entire observed speed of the slowest solar wind streams. On the other hand, neither class of model can explain the observed speed of the faster solar wind streams, which thus require additional acceleration mechanisms.

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