Abstract

How turbulent energy is dissipated in weakly collisional space and astrophysical plasmas is a major open question. Here, we present the application of a field-particle correlation technique to directly measure the transfer of energy between the turbulent electromagnetic field and electrons in the Earth’s magnetosheath, the region of solar wind downstream of the Earth’s bow shock. The measurement of the secular energy transfer from the parallel electric field as a function of electron velocity shows a signature consistent with Landau damping. This signature is coherent over time, close to the predicted resonant velocity, similar to that seen in kinetic Alfven turbulence simulations, and disappears under phase randomisation. This suggests that electron Landau damping could play a significant role in turbulent plasma heating, and that the technique is a valuable tool for determining the particle energisation processes operating in space and astrophysical plasmas

Various physical mechanisms are proposed to explain the heating observed in turbulent astrophysical plasmas. Here, Chen et al. find a signature consistent with one of these mechanisms, electron Landau damping, by applying a field-particle correlation technique to in situ spacecraft data of turbulence in the Earth’s magnetosheath.

Details

Title
Evidence for electron Landau damping in space plasma turbulence
Author
Chen C H K 1 ; Klein, K G 2 ; Howes, G G 3   VIAFID ORCID Logo 

 Queen Mary University of London, School of Physics and Astronomy, London, UK (GRID:grid.4868.2) (ISNI:0000 0001 2171 1133) 
 University of Arizona, Lunar and Planetary Laboratory, Tucson, USA (GRID:grid.134563.6) (ISNI:0000 0001 2168 186X) 
 University of Iowa, Department of Physics and Astronomy, Iowa City, USA (GRID:grid.214572.7) (ISNI:0000 0004 1936 8294) 
Publication year
2019
Publication date
Dec 2019
Publisher
Nature Publishing Group
e-ISSN
20411723
Source type
Scholarly Journal
Language of publication
English
ProQuest document ID
2180984478
Copyright
This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.