Energy flux in the Earth's magnetosphere: Storm - Substorm relationship

被引:4
|
作者
Alexeev, II [1 ]
机构
[1] Moscow MV Lomonosov State Univ, Scobeltsyn Inst Nucl Phys, Moscow 119992, Russia
关键词
magnetospheric energy; solar wind-magnetosphere interactions;
D O I
10.1023/A:1025519622160
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Three ways of the energy transfer in the Earth's magnetosphere are studied. The solar wind MHD generator is an unique energy source for all magnetospheric processes. Field-aligned currents directly transport the energy and momentum of the solar wind plasma to the Earth's ionosphere. The magnetospheric lobe and plasma sheet convection generated by the solar wind is another magnetospheric energy source. Plasma sheet particles and cold ionospheric polar wind ions are accelerated by convection electric field. After energetic particle precipitation into the upper atmosphere the solar wind energy is transferred into the ionosphere and atmosphere. This way of the energy transfer can include the tail lobe magnetic field energy storage connected with the increase of the tail current during the southward IMF. After that the magnetospheric substorm occurs. The model calculations of the magnetospheric energy give possibility to determine the ground state of the magnetosphere, and to calculate relative contributions of the tail current, ring current and field-aligned currents to the magnetospheric energy. The magnetospheric substorms and storms manifest that the permanent solar wind energy transfer ways are not enough for the covering of the solar wind energy input into the magnetosphere. Nonlinear explosive processes are necessary for the energy transmission into the ionosphere and atmosphere. For understanding a relation between substorm and storm it is necessary to take into account that they are the concurrent energy transferring ways.
引用
收藏
页码:141 / 148
页数:8
相关论文
共 50 条
  • [31] Electron dynamics during substorm dipolarization in Mercury's magnetosphere
    Delcourt, DC
    Seki, K
    Terada, N
    Miyoshi, Y
    ANNALES GEOPHYSICAE, 2005, 23 (10) : 3389 - 3398
  • [32] Magnetic Flux Transport Identification of Active Reconnection: MMS Observations in Earth's Magnetosphere
    Qi, Yi
    Li, Tak Chu
    Russell, Christopher T.
    Ergun, Robert E.
    Jia, Ying-Dong
    Hubbert, Mark
    ASTROPHYSICAL JOURNAL LETTERS, 2022, 926 (02)
  • [33] Dependence of the near-Earth magnetotail magnetic field on storm and substorm activities
    Nakai, H
    Kamide, Y
    Russell, CT
    JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1999, 104 (A10) : 22701 - 22711
  • [34] Open flux in Saturn's magnetosphere
    Badman, Sarah V.
    Jackman, Caitriona M.
    Nichols, Jonathan D.
    Clarke, John T.
    Gerard, Jean-Claude
    ICARUS, 2014, 231 : 137 - 145
  • [35] Kinetic models of magnetic flux ropes observed in the Earth magnetosphere
    Vinogradov, A. A.
    Vasko, I. Y.
    Artemyev, A. V.
    Yushkov, E. V.
    Petrukovich, A. A.
    Zelenyi, L. M.
    PHYSICS OF PLASMAS, 2016, 23 (07)
  • [36] Dynamics of the Jovian electron flux in solar activity cycle 21 near the Earth's magnetosphere
    Skryabin, NG
    Bezrodnykh, IP
    Plotnikov, IY
    Ivanov, OP
    GEOMAGNETISM AND AERONOMY, 2001, 41 (04) : 432 - 435
  • [37] ELECTRIC-FIELDS IN THE MAGNETOSPHERE AND ENERGY CHARACTERISTICS OF THE AURORAL SUBSTORM ACTIVE PHASE
    KORNILOVA, TA
    PUDOVKIN, MI
    STARKOV, GV
    GEOMAGNETIZM I AERONOMIYA, 1994, 34 (02): : 56 - 61
  • [38] On the Contribution of Dipolarizing Flux Bundles to the Substorm Current Wedge and to Flux and Energy Transport
    Birn, J.
    Liu, J.
    Runov, A.
    Kepko, L.
    Angelopoulo, V
    JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 2019, 124 (07) : 5408 - 5420
  • [39] Beams of high-energy electrons of atmospheric origin in the earth's magnetosphere
    Galper, A. M.
    Koldashov, S. V.
    COSMIC RESEARCH, 2007, 45 (05) : 452 - 454
  • [40] Beams of high-energy electrons of atmospheric origin in the Earth’s magnetosphere
    A. M. Galper
    S. V. Koldashov
    Cosmic Research, 2007, 45 : 452 - 454