2022
DOI: 10.1029/2021gl097620
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Depletions of Multi‐MeV Electrons and Their Association to Minima in Phase Space Density

Abstract: Earth's outer radiation belt is a region of geomagnetically confined electrons and can contain particles with multi-MeV energies. Changes in the flux of the multi-MeV populations may be reversible (i.e., adiabatic) or irreversible and can arise from a number of processes, including large-scale magnetic field fluctuations and wave-particle interactions. Analysis of phase space density (PSD) profiles (e.g.,

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Cited by 16 publications
(27 citation statements)
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“…The flux of relativistic electrons trapped in the Earth's Van Allen radiation belts can vary by several orders of magnitude in response to solar wind forcing (e.g., 1 ), and a number of wave-particle interactions have been proposed as contributing to the observed dynamics. For example, chorus waves are responsible for local acceleration (e.g., see [2][3][4][5][6][7][8][9][10][11] ), longer period ultra-low frequency (ULF) waves are responsible for particle acceleration as a result of inward radial diffusion (e.g., see [12][13][14][15][16][17][18][19][20][21] ), in addition to other wave-particle interactions such as electromagnetic ion-cyclotron (EMIC) waves that are responsible for loss of radiation belt electrons (e.g., see 22,23 ), manmade VLF transmitter waves (e.g., 24 ) and plasmaspheric hiss (e.g., 25 ) are also thought to be able to scatter the electrons into the loss cone and lead to the corresponding evolution of the electron flux. In this paper, we examine the chorus wave activity that accompanies a flux-limiting process in the inner magnetosphere that occurs during geomagnetic storms, and demonstrate that the theoretical predictions of Kennel and Petschek 26 accurately depict the behaviour of waves and electron fluxes in the outer Van Allen belt.Recent work associated with the capping of ~ 10-100 keV electron flux by Olifer et al 27 has revisited the dynamics of the energetic electron population in the outer electron radiation belt, revealing evidence for an energy-dependent limit to the electron flux in the belts (see also 28 , and references therein).…”
mentioning
confidence: 99%
“…The flux of relativistic electrons trapped in the Earth's Van Allen radiation belts can vary by several orders of magnitude in response to solar wind forcing (e.g., 1 ), and a number of wave-particle interactions have been proposed as contributing to the observed dynamics. For example, chorus waves are responsible for local acceleration (e.g., see [2][3][4][5][6][7][8][9][10][11] ), longer period ultra-low frequency (ULF) waves are responsible for particle acceleration as a result of inward radial diffusion (e.g., see [12][13][14][15][16][17][18][19][20][21] ), in addition to other wave-particle interactions such as electromagnetic ion-cyclotron (EMIC) waves that are responsible for loss of radiation belt electrons (e.g., see 22,23 ), manmade VLF transmitter waves (e.g., 24 ) and plasmaspheric hiss (e.g., 25 ) are also thought to be able to scatter the electrons into the loss cone and lead to the corresponding evolution of the electron flux. In this paper, we examine the chorus wave activity that accompanies a flux-limiting process in the inner magnetosphere that occurs during geomagnetic storms, and demonstrate that the theoretical predictions of Kennel and Petschek 26 accurately depict the behaviour of waves and electron fluxes in the outer Van Allen belt.Recent work associated with the capping of ~ 10-100 keV electron flux by Olifer et al 27 has revisited the dynamics of the energetic electron population in the outer electron radiation belt, revealing evidence for an energy-dependent limit to the electron flux in the belts (see also 28 , and references therein).…”
mentioning
confidence: 99%
“…The magnetopause erosion is however not as efficient for non‐geoeffective sheaths as for geoeffective sheaths (Kalliokoski et al., 2020), which could imply that in the inner parts of the outer belt scattering by wave‐particle interactions has a key role in causing losses. Electromagnetic ion cyclotron (EMIC) waves can scatter multi‐MeV electrons rapidly (Aseev et al., 2017; Drozdov et al., 2022; Kurita et al., 2018; Shprits et al., 2017; Usanova et al., 2014). This scattering loss can also contribute to losses during geoeffective sheaths during which EMIC wave activity is more elevated (Kalliokoski et al., 2020).…”
Section: Discussionmentioning
confidence: 99%
“…manuscript submitted to JGR: Space Physics interactions has a key role in causing losses. Electromagnetic ion cyclotron (EMIC) waves can scatter multi-MeV electrons rapidly (Usanova et al, 2014;Aseev et al, 2017;Shprits et al, 2017;Kurita et al, 2018;Drozdov et al, 2022). This scattering loss can also contribute to losses during geoeffective sheaths during which EMIC wave activity is more elevated (Kalliokoski et al, 2020).…”
Section: Accepted Articlementioning
confidence: 99%