EGU2020-20301
https://doi.org/10.5194/egusphere-egu2020-20301
EGU General Assembly 2020
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Non-adiabatic interaction of ions with solar wind discontinuities

Alexander Vinogradov1,2, Anton Artemyev1,3, Ivan Vasko1,4, Alexei Vasiliev1, and Anatoly Petrukovich1
Alexander Vinogradov et al.
  • 1Space Research Institute RAS, Space Plasma, Moscow, Russia
  • 2Higher School of Economics, Faculty of Physics, Moscow, Russia
  • 3University of California in Los Angeles, Los Angeles, USA
  • 4Space Sciences Laboratory, University of California, Berkeley, USA

According to Helios, Ulysses, New Horizons measurements at a wide range of distances from the Sun, radial evolution of solar wind ion temperature significantly deviates from the adiabatic expansion model:  additional heating of the solar wind plasma is required to describe observational data. Solution of the solar wind heating problem is extremely important both for understanding the structure of the heliosphere and for adequately describing the atmospheres of distant stars. Solar wind magnetic field is turbulent and this turbulence is dominated by numerous small-scale high-amplitude coherent structures – such as quasi-1D discontinuities. Modern theoretical models predict that quasi-1D discontinuities can play important role in solar wind heating. We collected the statistics of MMS observations of thin quasi-1D discontinuities in the solar wind to reveal their characteristics. Analyzing observational data, we construct the discontinuity model and use it to consider non-adiabatic interaction of ions with solar wind discontinuities. We mainly focus on discontinuity roles in solar wind ion scattering and thermalization. This presentation shows how discontinuity configuration affects the scattering rates.

How to cite: Vinogradov, A., Artemyev, A., Vasko, I., Vasiliev, A., and Petrukovich, A.: Non-adiabatic interaction of ions with solar wind discontinuities, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-20301, https://doi.org/10.5194/egusphere-egu2020-20301, 2020

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