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Model‐observation comparison study of multiple polar cap arcs
Author(s) -
Zhu L.,
Valladares C. E.,
Sojka J. J.,
Schunk R. W.,
Crain D. J.
Publication year - 1996
Publication title -
journal of geophysical research: space physics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/95ja02758
Subject(s) - polar , polar cap , ionosphere , arc (geometry) , magnetosphere , coupling (piping) , geophysics , photometer , precipitation , electrojet , electron precipitation , physics , geology , computational physics , atmospheric sciences , geometry , meteorology , earth's magnetic field , optics , magnetic field , materials science , mathematics , quantum mechanics , astronomy , metallurgy
A quantitative model‐observation comparison of multiple polar cap arcs has been conducted by using a time‐dependent theoretical model of polar cap arcs. In particular, the electrodynamical features of multiple polar cap arcs with various spacings are simulated and the results are compared with the images obtained from the All‐Sky Intensified Photometer at Qaanaaq. The results show that the observed and simulated arcs are quite similar, both spatially and temporally. The results support the theory proposed by Zhu et al. [1993a, 1994b] that the structure of polar cap arcs is mainly determined by the magnetosphere‐ionosphere (M‐I) coupling processes and that the spacing of multiple polar cap arcs is closely related to the hardness of the primary magnetospheric precipitation. It is found that for the multiple polar cap arcs with both narrow and wide spacings, the associated field‐aligned currents are mainly closed by Pedersen currents. It is also found that a hard precipitation can lead to a highly structured secondary arc because of the nonlinear M‐I coupling processes.

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