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A Semikinetic Model of Plasmasphere Refilling Following Geomagnetic Storms and Comparison With Hydrodynamic Results
Author(s) -
Chatterjee K.,
Schunk R. W.
Publication year - 2020
Publication title -
journal of geophysical research: space physics
Language(s) - English
Resource type - Journals
eISSN - 2169-9402
pISSN - 2169-9380
DOI - 10.1029/2020ja028016
Subject(s) - plasmasphere , kinetic energy , geomagnetic storm , physics , earth's magnetic field , mechanics , low altitude , particle (ecology) , flow (mathematics) , computational physics , statistical physics , altitude (triangle) , classical mechanics , magnetosphere , plasma , geology , magnetic field , mathematics , nuclear physics , oceanography , geometry , quantum mechanics
The objective of this paper is the development of a kinetic model for plasmasphere refilling following geomagnetic storms. The kinetic model is based on the “particle‐in‐cell” method, a method based on the simulation of particle motion and thus well suited to high altitude, low‐density regimes, where the plasma transport equations are not valid. The model was validated with exact, analytical benchmarks, which are provided in this paper. The refilling results obtained from the kinetic model were then compared with results from a recently developed hydrodynamic solution methodology based on the “flux‐corrected transport” method, and the limitations of hydrodynamic modeling for low‐density flow at high altitudes were explored.