Statistics and Models of the Electron Plasma Density From the Van Allen Probes

Author:

Ripoll J.‐F.12ORCID,Thaller S. A.34,Hartley D. P.5ORCID,Malaspina D. M.36ORCID,Kurth W. S.5ORCID,Cunningham G. S.7ORCID,Pierrard V.89ORCID,Wygant J.10ORCID

Affiliation:

1. CEA DAM DIF Arpajon France

2. UPS CEA LMCE Bruyères‐le‐Châtel France

3. Laboratory for Atmospheric and Space Physics University of Colorado, Boulder Boulder CO USA

4. Now at Orion Space Solutions An Arcfield Company Louisville CO USA

5. Department of Physics and Astronomy University of Iowa Iowa City IA USA

6. Astrophysical and Planetary Sciences Department University of Colorado, Boulder Boulder CO USA

7. Space Science and Applications Group Los Alamos National Laboratory Los Alamos NM USA

8. Department Space Physics and Solar‐Terrestrial Center of Excellence Royal Belgian Institute for Space Aeronomy Brussels Belgium

9. Center for Space Radiations Earth and Life Institute ‐ Climate Sciences (ELIC) Université Catholique de Louvain Louvain‐La‐Neuve Belgium

10. School of Physics and Astronomy University of Minnesota Minneapolis MN USA

Abstract

AbstractWe use the full NASA Van Allen Probes mission (2012–2019) to extract the electron plasma density from the Electric and Magnetic Field Instrument Suite and Integrated Science (EMFISIS) and Electric Field and Waves (EFW) instruments and discuss the evolution of the plasmasphere. We generate new statistics including mean and standard deviations of the plasma density with respect to L‐shell, magnetic local time (MLT), and various geomagnetic indices. These statistics are generated to be applied in radiation belt physics and space weather codes (with fits provided). The mean plasmasphere is circular around Earth with respect to MLT for Kp < 1. The mean 100 cm−3 level line is above L = 5 and mean 10 cm−3 level expands above the Van Allen Probes apogee for Kp < 1. The outer electron belt lies within the plasmasphere for 60% of all times. As activity increases (Kp > 2), a gradual MLT asymmetry forms with higher mean density in the afternoon sector due to plumes expanding outward. Conversely, the mean density decreases on the dawn and night sectors. The mean density is between ∼500 and ∼50 cm−3 between L ∼ 4 and L ∼ 6 during quiet and moderately active times (Kp < 3), representing ∼80% of all times. Statistics in regions of high density below L = 2 are underdefined for intense activity. The highest standard deviation of density represents a factor 2.5 to 3 times the mean above L = 5 and for active times. We find the percent difference between the EFW and EMFISIS densities is bounded by ±20% for quiet and moderate activity (Kp < 5) and goes up to ±100% for extreme activity.

Publisher

American Geophysical Union (AGU)

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