Where is the magnetic energy for the expansion phase of auroral substorms accumulated?

被引:19
作者
Akasofu, Syun-Ichi [1 ]
机构
[1] Univ Alaska, Int Arctic Res Ctr, Fairbanks, AK 99775 USA
关键词
substorms; FIELD; RECONNECTION; MODEL; CURRENTS; INPUT; ONSET; TAIL;
D O I
10.1002/2013JA019042
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Characteristics of the ionospheric current system (the directly driven (DD) / unloading (UL) currents) and the power epsilon during auroral substorms are examined semiquantitatively in terms of input-output relationship. The study confirms (a) The magnetic energy for the expansion phase is accumulated with the rate of a little more than 10(18) erg/s during the growth phase which lasts for about 1h (because the ionosphere cannot dissipate the input power). (b) The global energy dissipation rate in the ionosphere (including the Joule heat production and the particle precipitation) is more than 3.3x10(18) erg/s. (c) Thus, the total energy consumption by the ionosphere during the impulsive expansion phase (lasting for about 1h) is 1.2x10(22) erg or up to 10(23) erg for medium substorms. (d) However, it is shown that even the total magnetic energy in the magnetotail at a distance between 10 R-E and 20 R-E (6.5x10(21) ergs=6.5x10(14)J) cannot supply the energy for the expansion phase. This estimate is consistent with the most recent satellite observations (4.3x10(13) J (= 4.3x10(20) ergs)). Thus, the following conclusions may be applicable for medium intensity substorms: (i) The major part of the magnetic energy for the expansion phase must be accumulated within a distance of 10 R-E and be released almost totally during the expansion phase (because the duration of the growth phase and the expansion phase is about the same). (ii) This suggests that there is an upper limit of the energy which the magnetosphere can accumulate even at distances less than 10 R-E. Further, it is confirmed that: (a) The expansion phase is characterized by a single cell current system UL (not a twin cell current system DD which is driven by the earthward plasma convection from the magnetotail). (b) The UL current is independent of the DD current, requiring a different origin. (c) During the recovery phase, the UL current is absent and the DD current approximately follows epsilon (no accumulation of the energy), because the ionosphere is capable of dissipating the power even if the power is moderate). (d) Based on these results, as an example, one possible chain of processes within 10 R-E is proposed as the release process of the accumulated magnetic energy by taking into account the fact that the frozen-in field condition is observed to be broken down.
引用
收藏
页码:7219 / 7225
页数:7
相关论文
共 31 条
[1]   THE AURORAL ENERGY DEPOSITION OVER THE POLAR IONOSPHERE DURING SUBSTORMS [J].
AHN, BH ;
KROEHL, HW ;
KAMIDE, Y ;
GORNEY, DJ ;
AKASOFU, SI ;
KAN, JR .
PLANETARY AND SPACE SCIENCE, 1989, 37 (03) :239-252
[2]   THE JOULE HEAT-PRODUCTION RATE AND THE PARTICLE ENERGY INJECTION RATE AS A FUNCTION OF THE GEOMAGNETIC INDICE-AE AND INDICE-AL [J].
AHN, BH ;
AKASOFU, SI ;
KAMIDE, Y .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1983, 88 (NA8) :6275-6287
[3]   The relationship between the magnetosphere and magnetospheric/auroral substorms [J].
Akasofu, S. -I. .
ANNALES GEOPHYSICAE, 2013, 31 (03) :387-394
[4]   The choice of the concept of magnetic field lines or of electric current lines: Alfven medal lecture [J].
Akasofu, S. -I. .
ANNALES GEOPHYSICAE, 2011, 29 (07) :1215-1232
[5]   LARGE-SCALE AURORAL MOTIONS AND POLAR MAGNETIC DISTURBANCES .1. A POLAR DISTURBANCE AT ABOUT 1100 HOURS ON 23 SEPTEMBER 1957 [J].
AKASOFU, SI .
JOURNAL OF ATMOSPHERIC AND TERRESTRIAL PHYSICS, 1960, 19 (01) :10-&
[6]   A CONFIRMATION OF THE VALIDITY OF THE ELECTRIC-CURRENT DISTRIBUTION DETERMINED BY A GROUND-BASED MAGNETOMETER NETWORK [J].
AKASOFU, SI .
GEOPHYSICAL JOURNAL INTERNATIONAL, 1992, 109 (01) :191-196
[7]   Several 'controversial' issues on substorms [J].
Akasofu, SI .
SPACE SCIENCE REVIEWS, 2004, 113 (1-2) :1-40
[8]   POLAR ELECTROJET [J].
AKASOFU, SI ;
CHAPMAN, S ;
MENG, CI .
JOURNAL OF ATMOSPHERIC AND TERRESTRIAL PHYSICS, 1965, 27 (11-1) :1275-&
[9]   Importance of auroral features in the search for substorm onset processes [J].
Akasofu, Syun-Ichi ;
Lui, A. T. Y. ;
Meng, C. -I. .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 2010, 115
[10]   Tail reconnection triggering substorm onset [J].
Angelopoulos, Vassilis ;
McFadden, James P. ;
Larson, Davin ;
Carlson, Charles W. ;
Mende, Stephen B. ;
Frey, Harald ;
Phan, Tai ;
Sibeck, David G. ;
Glassmeier, Karl-Heinz ;
Auster, Uli ;
Donovan, Eric ;
Mann, Ian R. ;
Rae, I. Jonathan ;
Russell, Christopher T. ;
Runov, Andrei ;
Zhou, Xu-Zhi ;
Kepko, Larry .
SCIENCE, 2008, 321 (5891) :931-935