PROBLEMS OF GEOCOSMOS

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Proceedings of the 7th International Conference "Problems of Geocosmos" (St. Petersburg, Russia, 26-30 May 2008) (1) the dipole that consists of a pair of positive and negative potentials at the western and eastern boundaries of the near-epicentral area (Fig. 3, dip1); (2) the dipole elongated in the meridianal direction for ~1500 km (Fig. 3, dip2); (3) the point monopole charge that consists of one positive charge at the epicenter (Fig. 3, mono1); (4) the fulfilled rectangular regions of positive charges (Fig. 3, mono2-mono3); (5) positive charged (equipotent) straight lines of different directions (Fig. 3, mono4-mono6). ϕ 30 02 UT ϕ 30 02 UT ϕ 30 02 UT 20 20 20 10 10 10 0 0 0 -10 -10 -10 -20 -20 -20 -30 -30 -30 -40 -40 -40 -50 -90 -80 -70 -60 λ -50 -90 -80 -70 -60 λ -50 -90 -80 -70 -60 λ 20.09 21.09 22.09 02 UT 02 UT 02 UT ϕ 30 ϕ 30 ϕ 30 20 20 20 10 10 10 0 0 0 -10 -10 -10 -20 -20 -20 -30 -30 -30 -40 -40 -40 -50 -50 -90 -80 -70 -60 λ -50 -90 -80 -70 -60 λ -90 -80 -70 -60 λ 23.09 24.09 25.09 ϕ 30 02 UT ϕ 30 02 UT ϕ 30 02 UT 20 20 20 10 10 10 0 0 0 -10 -10 -10 -20 -20 -20 -30 -30 -30 -40 -40 -40 -50 -90 -80 -70 -60 λ EQ day -50 -90 -80 -70 -60 λ -50 -90 -80 -70 -60 λ 26.09 27.09 28.09 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90 100 % Fig. 1. TEC diff. (%) maps at 02 UT for September 20-28, 2005 relative to the none-disturbed conditions. Black spot – the earthquake epicenter position. Kp Ap Dst, nT 0.5 0 1 1.5 2 2.5 3 3.5 4 4.5 5 01 08 15 22 EQ 29 40 35 30 25 20 15 10 5 0 01 08 15 22 EQ 29 50 0 -50 -100 -150 -200 01 08 15 22 EQ 29 Fig. 2. Dst-, Ap- and Kp- indexes for the September, 2005. EQ – the earthquake day. 493
Proceedings of the 7th International Conference "Problems of Geocosmos" (St. Petersburg, Russia, 26-30 May 2008) Fig. 3. Numerical grid and additional electric field sources: plus for positive sources, minus – for negative ones, grey points – not modified nodes. Fig. 4. Latitudinal variations of the electric potential (top left panel), the eastern component of the electric field (top right panel) and corresponding TEC variations (%) (bottom panel). Red line (top panels) stand for the none-disturbed level. 494
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vertical fields. The vertical field
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a Proceedings of the 7th Internatio
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Introduction ON THE NATURE OF PLASM
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Vy Here index j =1,2 characterizes,
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Fig. 3. Dependence of 1D interpreta
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Page 494 and 495: 2. Burlaga & Klein method. The main
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PROBLEMS OF GEOCOSMOS

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