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The Jovian magnetotail

Advances in Space Research, 1986
The current understanding of the plasma, magnetic field, and plasma wave characteristics of the near and distant Jovian magnetotail is discussed. The properties of these two regions are compared, with particular emphasis given to the data on the distant tail obtained by Voyager 2.
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The magnetotail of Uranus

Journal of Geophysical Research: Space Physics, 1987
Voyager 2 observations have shown that Uranus possesses a well‐developed bipolar magnetotail similar in certain characteristics to that of Earth, in spite of an anomalously large tilt of the planetary magnetic dipole to the rotation axis at Uranus. The intensity of the magnetic field in the tail lobes decreases with increasing distance down the tail ...
K. W. Behannon   +6 more
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Flows in the Magnetotail

2020
<p>Magnetic reconnection leads to fast streaming of electrons and ions away from the reconnection site. We have used an implicit particle-in-cell simulation (iPic3D) embedded within a global MHD simulation of the solar wind and magnetosphere interaction to investigate the evolution of electrons and ion flows in the magnetotail ...
Raymond Walker   +5 more
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Plasmas in the Earth’s Magnetotail

Space Science Reviews, 1985
An overview of the general characteristics of plasmas within the Earth’s magnetotail and its environs is presented. Present knowledge of the plasmas within these regions as gained via in situ measurements provides the general theme, although observations of magnetic fields, energetic particles and plasma waves are included in the discussion.
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The magnetotail and substorms

Space Science Reviews, 1973
The tail plays a very active and important role in substorms. Magmetic flux eroded from the dayside magnetosphere is stored here. As more and more flux is transported to the magnetotail and stored, the boundary flares more, the field strength in the tail increases, and the currents strengthen and move closer to the earth.
C.T. Russell, R.L. McPherron
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The Earth's Dynamic Magnetotail

Space Science Reviews, 2000
Geomagnetic field lines that are stretched on the nightside of the Earth due to reconnection with the interplanetary magnetic field constitute the Earth's magnetotail. The magnetotail is a dynamic entity where energy imparted from the solar wind is stored and then released to generate disturbance phenomena such as substorms. This paper gives an updated
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Particle chaos in the Earth’s magnetotail

Chaos: An Interdisciplinary Journal of Nonlinear Science, 1992
Nonlinear particle dynamics is studied both in current sheets and near neutral lines. The parameter governing particle chaos in a current sheet with a constant normal component, Bn, is κ=(Rmin/ρmax)1/2, where Rmin is the minimum field line radius of curvature and ρmax is the maximum gyroradius.
Paul B., Dusenbery   +2 more
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Reconnection in the magnetotail

Space Science Reviews, 1979
The ion tearing mode is considered as the only mechanism capable of initiating reconnection processes in the equilibrium plasma sheet whose scale considerably exceeds the ion Larmor radius. The paper gives a brief review of linear theory of the tearing mode instability that allows the onset of its development to be determined.
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Energetic Particles in the Jovian Magnetotail

Science, 2007
When the solar wind hits Jupiter's magnetic field, it creates a long magnetotail trailing behind the planet that channels material out of the Jupiter system. The New Horizons spacecraft traversed the length of the jovian magnetotail to >2500 jovian radii ( R J ; 1 R J
R L, McNutt   +19 more
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Relaxation of magnetotail plasmas

Journal of Geophysical Research: Space Physics, 1987
A quasi‐thermodynamic model is presented for the relaxation of magnetotail plasmas during substorms, followed by quiet times. It is proposed that the plasma relaxes to a state of low‐potential energy subject to a small number of global constraints.
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