Physics of auroral phenomena : proceedings of the 38th annual seminar, Apatity, 2-6 march, 2015 / [ed. board: A. G. Yahnin, N. V. Semenova]. - Апатиты : Издательство Кольского научного центра РАН, 2015. - 189 с. : ил., табл.

Field-aligned current dynamics during two substorms 3. Summary 1. From the data on the 2000 April 6 two selected events, we calculated the maps for FAC density distribution in the polar ionosphere of the Northern Hemisphere. In each event, sufficient signatures of expansion phase were observed. In one of them, we describe the EP type termed "summer," and the one termed "winter" in the other event. 2. We propose a scenario for the global EP, where this substorm phase evolves simultaneously in the summer and winter hemispheres, but in different MLT sectors of the nightside Rl offered: the winter (summer) type EP is observed in the Rl postmidnight (premidnight) sector. These two sectors are within the ~ (18-06) MLT interval, and their centers are separated by ~ 6 MLT. 3. We substantiated the conclusion that the M-I feedback instability in the Rl premidnight sector of the summer hemisphere serves as an initiator and an organizer of the global EP. 4. In the winter hemisphere, a collapse (a decrease in the downward FAC intensity) of the Rl premidnight sector FAC system evolves simultaneously with the EP of the postmidnight sector. We describe the physics of this collapse within the model for the electric circuit of the common current system in the global EP M-I system. 5. We described the phenomena of spontaneous reconfiguration of the FAC density and intensity distribution in Rl and other Iijima and Potemra Regions. The reconfiguration is observed as a variation in the FAC density and intensity distributions in I-P Regions. These variations produce an expansion/compression of the downward FAC sector due to a compression/expansion of the upward FAC in the adjacent sector of the same Region. These phenomena are described in terms of azimuthal "twisting" of the FAC density spatial distribution in each I-P Region (clockwise or counter-clockwise). 6. We propose a conceptual model for twisting phenomena based on the supplemented model from Lui and Kamide [2003]. In general, we suggest an empirical scenario for the global EP involving principally new elements, as compared with the known substorm scenarios. We introduced the new elements based on combining the data on two hemispheres, winter and summer, within a uniform model for the electric circuit of the M-I current system. Unlike such an approach, the known empirical substorm scenarios are primarily made on the database for the Northern Hemisphere. In this case, the strong asymmetry of two hemispheres - the key element of the proposed EP scenario - is not taken into account. Acknowledgements. We thank the ISTP SB RAS MIT group members for stimulating discussions. The AE index was obtained from the World Data Center for Geomagnetism, Kyoto. We are grateful to Pis o f the CANOPUS, INTERMAGNET, GIMA, MACCS, IMAGE projects and o f magnetic networks in Arctic and the Antarctic (the Shafer Institute o f Cosmo-Physical Research and Aeronomy SB RAS, Arctic and Antarctic Research Institute, and DMI), and individual magnetic observatories for providing magnetic data used in this study. Work was supported by the RFBR under Grants 14-05-91165 and 15-05-05561. References Akasofu SI (2013) The relationship between the magnetosphere and magnetospheric/auroral substorms. Ann Geophys 31 (3):387-394. doi:10.5194/angeo-31-387-2013 Angelopoulos V, McFadden JP, Larson D, Carlson CW, Mende SB, Frey H, Phan T, Sibeck DG, Glassmeier KH, Auster U, Donovan E, Mann 1R, Rae IJ, Russell CT, Runov A, Zhou XZ, Kepko L (2008) Tail reconnection triggering substorm onset. Science 321 (5891):931-935. doi: 10.1126/science. 1160495 Baker DN, Pulkkinen TI, Angelopoulos V, Baumjohann W, McPherron RL (1996) Neutral line model of substorms: Past results and present view. J Geophys Res 101 (A6): 12975-13010. doi:10.1029/95ja03753 Kissinger J, McPherron RL, Hsu TS, Angelopoulos V (2012) Diversion of plasma due to high pressure in the inner magnetosphere during steady magnetospheric convection. J Geophys Res 117 (A5):A05206. doi:10.1029/2012ja017579 Knipp DJ, Emery BA, Richmond AD, Crooker NU, et al. (1993) Ionospheric convection response to slow, strong variations in a northward interplanetary magnetic field: A case study for January 14, 1988. J Geophys Res 98 (A l 1): 19273-19292. doi: 10.1029/93ja01010 Laundal KM, 0stgaard N (2009) Asymmetric auroral intensities in the Earth/'s Northern and Southern hemispheres. Nature 460 (7254):491 -493. doi: 10.1038/nature08154 Lu G, Li WH, Raeder J, Deng Y, Rich F, Ober D, Zhang YL, Paxton L, Ruohoniemi JM, Hairston M, Newell P (2011) Reversed two-cell convection in the Northern and Southern hemispheres during northward interplanetary magnetic field. J Geophys Res 116 (A12):A12237. doi: 10.1029/201 ljaO 17043 Lui ATY (1996) Current disruption in the Earth's magnetosphere: Observations and models. J Geophys Res 101 (A6):13067-13088. doi:10.1029/96ja00079 McPherron RL, Russell CT, Aubry MP (1973) Satellite studies of magnetospheric substorms on August 15, 1968: 9. Phenomenological model for substorms. J Geophys Res 78 (16):3131-3149. doi:10.1029/JA078i016p03131 Mishin VV et al (2015a) Positive feedback between ionosphere conductivity and field-aligned current intensity//Earth Planets Space (submitted) Mishin VV et al (2015b) Versions of model for the solar wind-magnetosphere-ionosphere global electric circuit in substorms o f summer and winter seasons// Earth Planets Space (submitted) Mishin VM et al. (2015c) Field-aligned current dynamics in two selected intervals of the 6 april 2000 superstorm. This issue. 0stgaard N, Laundal KM, Juusola L, Asnes A, H<1and SE, Weygand JM (2011) Interhemispherical asymmetry o f substorm onset locations and the interplanetary magnetic field. Geophys Res Lett 38 (8):L08104. doi:10.1029/201 lgl046767 Pellinen RJ, Heikkila WJ (1978) Energization o f Charged Particles to High Energies by an Induced Substorm Electric Field within the Magnetotail. J Geophys Res 83 (A4): 1544-1550. doi:10.1029/JA083iA04p01544 Potemra ТА (1994) Sources of Large-Scale Birkeland Currents. In: Holtet J, Egeland A (eds) Physical Signatures o f Magnetospheric Boundary Layer Processes, vol 425. NATO ASI Series. Springer Netherlands, pp 3-27. doi: 10.1007/978-94-011-1052-5_1 Reistad JP, Ostgaard N, Laundal KM, Haaland S, Tcnfjord P, Snekvik K, Oksavik K, Milan SE (2014) Intensity asymmetries in the dusk sector of the poleward auroral oval due to IMFBx. J Geophys Res Space Physics 119 (12):9497-9507. doi:10.1002/2014ja020216 31

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