Observations and Simulations of Dropout Events and Flux Decays in October 2013: Comparing MEO Equatorial With LEO Polar Orbit. Issue 6 (3rd June 2021)

• Record Type: Journal Article
• Authors: Pierrard, Viviane; Ripoll, Jean‐Francois; Cunningham, Gregory; Botek, Edith; Santolik, Ondrej; Thaller, Scott; Kurth, William S.; Cosmides, Mélanie
• Is Part Of: Journal of geophysical research. Volume 126:Issue 6(2021)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2021-06-03
• Subjects: energetic particles -- geomagnetic storms -- radiation belts -- relativistic electrons; Magnetospheric physics -- Periodicals; Space environment -- Periodicals; Cosmic physics -- Periodicals; Planets -- Atmospheres -- Periodicals; Heliosphere (Astrophysics) -- Periodicals; Geophysics -- Periodicals; 523.01
• DOI: 10.1029/2020JA028850
• Languages: English
• ISSNs: 2169-9380

Abstract

Abstract: We compare ESA PROBA‐V observations of electron flux at LEO with those from the NASA Van Allen Probes mostly at MEO for October 2013. Dropouts are visible at all energy during four storms from both satellites. Equatorially trapped electron fluxes are higher than at LEO by 10 2 (<1 MeV) to 10 5 (>2.5 MeV). We observe a quite isotropic structure of the outer belt during quiet times, contrary to the inner belt, and pitch angle dependence of high energy injection. We find a very good overlap of the outer belt at MEO and LEO at ∼0.5 MeV. We use test‐particle simulations of the energetic electrons trapped in the terrestrial magnetic field to study the outer radiation belt electron flux changes during geomagnetic storms. We show that the Dst (Disturbance storm time) effect during the main phase of a geomagnetic storm results in a betatron mechanism causing outward radial drift and a deceleration of the electrons. This outward drift motion is energy independent, pitch angle‐dependent, and represents a significant distance (∼1 L‐shell at L = 5 for moderate storms). At fixed L‐shell, this causes a decay of the LEO precipitating flux (adiabatic outward motion), followed by a return to the normal state (adiabatic inward motion) during main and recovery phases. Dst effect, associated with magnetopause shadowing and radial diffusion can explain the main characteristics of outer radiation belt electron dropouts in October 2013. We also use Fokker‐Planck simulations with event‐driven diffusion coefficients at high temporal resolution, to distinguish instantaneous loss from the gradual scattering that depopulates the slot region and the outer belt after storms. Simulations reproduce the slot formation and the gradual loss in the outer belt. The typical energy dependence of these losses leads to the absence of scattering for relativistic and ultra‐relativistic electrons in the outer belt, oppositely to dropouts. Plain Language Summary: We compare observations of electron flux in the radiation belts at Low Earth Orbit with those at Medium Earth Orbit for October 2013. Four storms are observed with dropouts followed by flux enhancements. We show that the dropouts are due to the loss of electrons at the magnetopause while gradual decays after storms are more due to wave‐particle interactions. Key Points: Simulations reproduce effects of magnetic field modification on the motion of electrons during geomagnetic storms The simulations help to understand the comparison of electron fluxes measured by EPT at LEO with those of MagEIS close to the equator The data indicate that the dropouts are due to magnetopause shadowing while other flux variations are associated to waves