摘要: Abstract The Martian magnetosphere is immersed in the neutral corona of planet. This leads to direct interaction solar wind with atmosphere. IMF strongly controls mass-loading upstream region providing a distinct asymmetry. Inside bow shock process becomes more effective leading formation new plasma boundary (MLB).
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sci-hub.se 参考文章(10)
R. Lundin, A. Zakharov, R. Pellinen, H. Borg, B. Hultqvist, N. Pissarenko, E. M. Dubinin, S. W. Barabasj, I. Liede, H. Koskinen, Plasma composition measurements of the Martian magnetosphere morphology Geophysical Research Letters. ,vol. 17, pp. 877- 880 ,(1990) , 10.1029/GL017I006P00877
H Rosenbauer, N Shutte, I Apathy, A Galeev, K Gringauz, H Grünwaldt, P Hemmerich, K Jockers, P Kiraly, G Kotova, S Livi, E Marsch, A Richter, W Riedler, T Remizov, R Schwenn, K Schwingenschuh, M Steller, K Szegö, M Verigin, M Witte, None, Ions of martian origin and plasma sheet in the martian magnetosphere: initial results of the TAUS experiment Nature. ,vol. 341, pp. 612- 614 ,(1989) , 10.1038/341612A0
K. Sauer, T. Roatsch, U. Motschmann, K. Schwingenschuh, R. Lundin, H. Rosenbauer, S. Livi, Observations of plasma boundaries and phenomena around Mars with Phobos 2 Journal of Geophysical Research. ,vol. 97, pp. 6227- 6233 ,(1992) , 10.1029/91JA02972
E Dubinin, D Obod, R Lundin, K Schwingenschuh, R Grard, Some features of the Martian bow shock Advances in Space Research. ,vol. 15, pp. 423- 431 ,(1995) , 10.1016/0273-1177(94)00127-M
E. Dubinin, R. Lundin, K. Schwingenschuh, Solar wind electrons as tracers of the Martian magnetotail topology Journal of Geophysical Research. ,vol. 99, pp. 21233- 21240 ,(1994) , 10.1029/94JA01271
M. I. Verigin, K. I. Gringauz, G. A. Kotova, A. P. Remizov, N. M. Shutte, H. Rosenbauer, S. Livi, A. Richter, W. Riedler, K. Schwingenschuh, K. Szegő, I. Apáthy, M. Tátrallyay, The dependence of the Martian magnetopause and bow shock on solar wind ram pressure according to Phobos 2 TAUS ion spectrometer measurements Journal of Geophysical Research. ,vol. 98, pp. 1303- 1309 ,(1993) , 10.1029/92JA01666
Konard Sauer, Alexander Bogdanov, Klaus Baumgärtel, Evidence of an ion composition boundary (protonopause) in bi-ion fluid simulations of solar wind mass loading Geophysical Research Letters. ,vol. 21, pp. 2255- 2258 ,(1994) , 10.1029/94GL01691
A. Pedersen, C. Nairn, R. Grard, K. Schwingenschuh, Derivation of electron densities from differential potential measurements upstream and downstream of the bow shock and in the magnetosphere of Mars Journal of Geophysical Research. ,vol. 96, pp. 11243- 11252 ,(1991) , 10.1029/91JA01098
M. I. Verigin, K. I. Gringauz, G. A. Kotova, N. M. Shutte, H. Rosenbauer, S. Livi, A. K. Richter, W. Riedler, K. Schwingenschuh, K. Szego, On the problem of the Martian atmosphere dissipation: Phobos: 2 TAUS Spectrometer results Journal of Geophysical Research. ,vol. 96, pp. 19315- 19320 ,(1991) , 10.1029/90JA02561
E. Dubinin, D. Obod, A. Pedersen, R. Grard, Mass‐loading asymmetry in upstream region near Mars Geophysical Research Letters. ,vol. 21, pp. 2769- 2772 ,(1994) , 10.1029/94GL02666