Using Van Allen Probes and Arase Observations to Develop an Empirical Plasma Density Model in the Inner Zone

Author:

Hartley D. P.1ORCID,Cunningham G. S.2ORCID,Ripoll J.‐F.34ORCID,Malaspina D. M.56ORCID,Kasahara Y.7ORCID,Miyoshi Y.8ORCID,Matsuda S.7ORCID,Nakamura S.8ORCID,Tsuchiya F.9ORCID,Kitahara M.9ORCID,Kumamoto A.9ORCID,Shinohara I.10ORCID,Matsuoka A.11

Affiliation:

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

2. Los Alamos National Laboratory Los Alamos NM USA

3. DAM DIF CEA Arpajon France

4. UPS CEA LMCE Bruyeres‐le‐Chatel France

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

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

7. Kanazawa University Kanazawa Japan

8. Nagoya University Nagoya Japan

9. Tohoku University Sendai Japan

10. JAXA Sagamihara Japan

11. Kyoto University Kyoto Japan

Abstract

AbstractA new empirical density model is developed for the inner zone between 1 < L < 3 using plasma densities inferred from the upper hybrid resonance on Arase, and hiss‐inferred density values from Van Allen Probes. The Van Allen Probes hiss‐inferred densities are first recalibrated and validated against Arase observations, using both a conjunction event and statistical analyses. The newly developed density model includes dependencies on L, magnetic latitude, and magnetic local time (MLT). Between 1.5 < L < 3.0, the equatorial density variation with L is shown to be equivalent to that of the Ozhogin et al. (2012, https://doi.org/10.1029/2011JA017330) model. However, for L < 1.5, this dependence changes as the plasma density increases at a faster rate with decreasing L. The latitudinal dependence of the plasma density is shown to present a flatter profile than previous models, meaning lower densities extend to higher latitudes. This dependence is well‐modeled by updated fitting coefficients. A clear MLT dependence of the plasma density is identified, which was not found or included in some previous models. This variation is consistent with the diurnal variation of the ionosphere, peaking near MLT = 14 and becoming larger in amplitude with decreasing L. A function describing this MLT dependence is presented. Overall, the new L, latitude, and MLT‐dependent empirical model can provide density values in areas outside the validity region of many previous models, making it a useful resource for accurately determining diffusion coefficients and predicting electron dynamics and their lifetimes in the inner radiation belt.

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Geophysics

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