EGU2020-11373
https://doi.org/10.5194/egusphere-egu2020-11373
EGU General Assembly 2020
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Magnetic mirror structures associated with magnetopause flux ropes investigated with Mangnetospheric Multiscale misson (MMS)

Sadie Robertson1, Jonathan Eastwood1, Julia Stawarz1, Heli Hietala1, Tai Phan2, Benoit Lavraud3, James Burch4, Barbra Giles5, Daniel Gershman5, Roy Torbert6, Per Arne Lindqvist7, Robert Ergun8, Christopher Russell9, and Robert Strangeway9
Sadie Robertson et al.
  • 1Imperial College London, Physics, United Kingdom of Great Britain and Northern Ireland (sadie.robertson14@imperial.ac.uk)
  • 2Space Sciences Laboratory, University of California, Berkeley, California 94720, USA
  • 3Institut de Recherche en Astrophysique et Planétologie, CNRS, UPS, CNES, Université de Toulouse, Toulouse, France
  • 4Southwest Research Institute, San Antonio, Texas 78238, USA
  • 5NASA, Goddard Space Flight Center, Greenbelt, Maryland 20771, USA
  • 6University of New Hampshire, Durham, New Hampshire 03824, USA
  • 7KTH Royal Institute of Technology, Stockholm, Sweden
  • 8LASP/Department of Astrophysical and Planetary Sciences, University of Colorado, Boulder, Colorado 80303, USA
  • 9Institute of Geophysics, Earth, Planetary, and Space Sciences, University of California, Los Angeles, Los Angeles, California 90095, USA

Magnetic reconnection is a fundamental plasma physics process which governs energy and mass transfer from the solar wind into the Earth’s magnetosphere. Electron acceleration during reconnection has been widely investigated with multiple mechanisms proposed. Many of these mechanisms involve flux ropes: twisted magnetic field structures formed during reconnection. Drake et al. 2006 suggest that contracting magnetic islands (or flux ropes in 3D) could trap and energise electrons by a Fermi acceleration process.

Whilst previous missions have observed and characterised flux ropes, the temporal resolution of the data was typically not great enough to study structures in detail, particularly on electron scales. Here we investigate magnetopause flux ropes using data from NASA’s four spacecraft Magnetospheric Multiscale mission (MMS). MMS measures the thermal electron and ion 3D distribution at 30 msec and 150 msec time resolution, respectively, and at spacecraft separations down to a few kilometers.

We focus on electron pitch angle distributions and examine how they can be used to investigate magnetopause flux ropes. In particular, the distributions are used to identify electron trapping in magnetic mirror structures on the magnetospheric edge of the flux ropes. These features are found to have extended 3D structure along the body of the flux rope. We evaluate possible formation mechanisms, such as the mirror instability, and potential electron acceleration mechanisms, such as betatron and Fermi acceleration. Magnetic mirror structures could represent an important particle acceleration feature for flux ropes and magnetic reconnection.

How to cite: Robertson, S., Eastwood, J., Stawarz, J., Hietala, H., Phan, T., Lavraud, B., Burch, J., Giles, B., Gershman, D., Torbert, R., Lindqvist, P. A., Ergun, R., Russell, C., and Strangeway, R.: Magnetic mirror structures associated with magnetopause flux ropes investigated with Mangnetospheric Multiscale misson (MMS), EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11373, https://doi.org/10.5194/egusphere-egu2020-11373, 2020

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