Subash Adhikari

Postdoctoral Researcher

Electron Dissipation and Electromagnetic Work


Journal article


Yan Yang, Subash Adhikari, William H. Matthaeus
Journal of Geophysical Research, Space Physics, vol. 129, 2024, pp. e2024JA033105


Cite

Cite

APA   Click to copy
Yang, Y., Adhikari, S., & Matthaeus, W. H. (2024). Electron Dissipation and Electromagnetic Work. Journal of Geophysical Research, Space Physics, 129, e2024JA033105. https://doi.org/10.1029/2024JA033105


Chicago/Turabian   Click to copy
Yang, Yan, Subash Adhikari, and William H. Matthaeus. “Electron Dissipation and Electromagnetic Work.” Journal of Geophysical Research, Space Physics 129 (2024): e2024JA033105.


MLA   Click to copy
Yang, Yan, et al. “Electron Dissipation and Electromagnetic Work.” Journal of Geophysical Research, Space Physics, vol. 129, 2024, p. e2024JA033105, doi:10.1029/2024JA033105.


BibTeX   Click to copy

@article{yan2024a,
  title = {Electron Dissipation and Electromagnetic Work},
  year = {2024},
  journal = {Journal of Geophysical Research, Space Physics},
  pages = {e2024JA033105},
  volume = {129},
  doi = {10.1029/2024JA033105},
  author = {Yang, Yan and Adhikari, Subash and Matthaeus, William H.}
}

Abstract

With the increase in technical capabilities of computer simulation in recent years, it has become feasible to quantify the degradation of fluid scale plasma and electromagnetic energies in favor of increases of internal energies. While it is understood that electromagnetic energy can be exchanged with fluid scale velocities, it is the pressure strain interaction that exchanges energy between fluid motions and internal energy. Here using simulations of both turbulence and reconnection we show that for electrons, the pressure strain and electromagnetic work are closely related and are frequently comparable when appropriate time and spatial averaging is applied. Otherwise, the instantaneous spatial averaged pressure strain and electromagnetic work are nearly equal for slowly evolving systems, like the reconnection case, while they differ significantly in rapidly evolving systems, like the turbulence case. This clarifies the relationship between these two quantities, which are each frequently used as measures of dissipation.