Particle scattering and current sheet stability in the geomagnetic tail during the substorm growth phase

1992 ◽  
Vol 97 (A12) ◽  
pp. 19283 ◽  
Author(s):  
T. I. Pulkkinen ◽  
D. N. Baker ◽  
R. J. Pellinen ◽  
J. Büchner ◽  
H. E. J. Koskinen ◽  
...  
Author(s):  
A. Runov ◽  
V. Angelopoulos ◽  
A.V. Artemyev ◽  
J.M. Weygand ◽  
S. Lu ◽  
...  

1994 ◽  
Vol 99 (A4) ◽  
pp. 5805 ◽  
Author(s):  
Jeff Sanny ◽  
R. L. McPherron ◽  
C. T. Russell ◽  
D. N. Baker ◽  
T. I. Pulkkinen ◽  
...  
Keyword(s):  

2009 ◽  
Vol 27 (1) ◽  
pp. 319-328 ◽  
Author(s):  
A. Runov ◽  
V. Angelopoulos ◽  
V. A. Sergeev ◽  
K.-H. Glassmeier ◽  
U. Auster ◽  
...  

Abstract. A sequence of magnetic field oscillations with an amplitude of up to 30 nT and a time scale of 30 min was detected by four of the five THEMIS spacecraft in the magnetotail plasma sheet. The probes P1 and P2 were at X=−15.2 and −12.7 RE and P3 and P4 were at X=−7.9 RE. All four probes were at −6.5>Y>−7.5 RE (major conjunction). Multi-point timing analysis of the magnetic field variations shows that fronts of the oscillations propagated flankward (dawnward and Earthward) nearly perpendicular to the direction of the magnetic maximum variation (B1) at velocities of 20–30 km/s. These are typical characteristics of current sheet flapping motion. The observed anti-correlation between ∂B1/∂t and the Z-component of the bulk velocity make it possible to estimate a flapping amplitude of 1 to 3 RE. The cross-tail scale wave-length was found to be about 5 RE. Thus the flapping waves are steep tail-aligned structures with a lengthwise scale of >10 RE. The intermittent plasma motion with the cross-tail velocity component changing its sign, observed during flapping, indicates that the flapping waves were propagating through the ambient plasma. Simultaneous observations of the magnetic field variations by THEMIS ground-based magnetometers show that the flapping oscillations were observed during the growth phase of a substorm.


1990 ◽  
Vol 17 (5) ◽  
pp. 583-586 ◽  
Author(s):  
D. G. Mitchell ◽  
D. J. Williams ◽  
C. Y. Huang ◽  
L. A. Frank ◽  
C. T. Russell

1997 ◽  
Vol 102 (A7) ◽  
pp. 14415-14424 ◽  
Author(s):  
X.‐Y. Zhou ◽  
C. T. Russell ◽  
J. T. Gosling ◽  
D. G. Mitchell

2003 ◽  
Vol 21 (12) ◽  
pp. 2259-2269 ◽  
Author(s):  
A. V. Manankova

Abstract. A problem concerning stationary configurations of an inhomogeneous, current-carrying, two-dimensional plasma sheet as the solution of the Grad–Shafranov equation with boundary conditions given on cross-sheet profiles at the  foot of the sheet and at infinity is considered, with the aim of using its solution for the description of the interaction of two current systems: the current system of the geomagnetic field, and the tail currents. The obtained solution is an exact analytical solution which contains 5 independent parameters characterizing the intensity of the current sheet. As the solution is exact, it may be applied to describe the most interesting transitional magnetospheric region: that of a strong interaction between the magnetic fields of the geodipole and of the current sheet, i.e. the region where characteristic scales of the change of all variables along and across the sheet are of the same order. This makes it possible to model the structure of the transitional region and its dynamics under quasi-stationary variation of the input parameters. The obtained solution describes the principal processes developing at various phases of magnetospheric disturbances, such as (1) formation of a very intense thin current sheet localized within the transition region, (2) changing from the quasi-dipolar magnetic field to the configuration when a "neck" is formed in this region. An important feature of the obtained solution is the existence of a critical value of one of the parameters of the problem, which leads to the change in the geomagnetic field configuration described above. The solution can be used as an initial condition in simulating dynamical processes in the magnetotail current sheet, as well as in testing the current sheet stability. In the summary a series of limitations in the model problem under consideration is discussed. Key words. Magnetospheric physics (magnetotail; plasma sheet; magnetospheric configuration and dynamics)


2017 ◽  
Vol 24 (8) ◽  
pp. 082903 ◽  
Author(s):  
Duo Zhao ◽  
Suiyan Fu ◽  
George K. Parks ◽  
Weijie Sun ◽  
Qiugang Zong ◽  
...  

1990 ◽  
Vol 95 (A4) ◽  
pp. 3819 ◽  
Author(s):  
V. A. Sergeev ◽  
P. Tanskanen ◽  
K. Mursula ◽  
A. Korth ◽  
R. C. Elphic

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