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Open AccessJournal ArticleDOI

Model study of plasmapause motion

J. M. Grebowsky
- 01 Aug 1970 - 
- Vol. 75, Iss: 22, pp 4329-4333
TLDR
The steady state plasmapause corresponds to the stagnation streamline in the E×B drift in the equatorial plane of the solar wind and the magnetosphere as discussed by the authors, and the model computations indicate that the spatial configuration of the plasmasphere can be very complex, especially near the bulge.
Abstract
The ambient plasma in the equatorial plane is predominantly subject to the E×B drift. By approximating the earth's magnetic field by a dipole, characteristic steady state streamlines in the equatorial plane are determined, assuming the interaction between the solar wind and the magnetosphere is characterized by a constant electric field directed from dawn to dusk in the equatorial plane. The steady state plasmapause corresponds to the stagnation streamline in this flow. If the magnitude of the dawn-dusk field is suddenly increased, the plasmasphere bulge moves toward the sun. By suddenly decreasing the magnitude of this field, the bulge can be made to corotate with the earth. The model computations indicate that the spatial configuration of the plasmapause can be very complex, especially near the bulge, because its position depends upon the past history of the magnetosphere.

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X-621-69-543
PREPRINT
NASA X- (3413
MODEL STUDY OF PLASMAPAUSE
MOTION
J. M. GREBOWSKY
DECEMBER 1969
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GODDARD SPACE FLIGHT
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MODEL STUDY OF PLASMIAPAUSE MOTION
J. M.
Grebowsky
LabGratory for Atmospheric and Biological Sciences
December 1969
GODDARD SPACE FLIGHT CENTER
GreenWlt, Maryland

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CONTENTS
Page
ABSTRACT
.......................................................
iii
INTRODUCTION...................................................
1
STEA
DY
STATE MODEL ..........................................
2
TIME DEPENDENT MODEL .......................................
5
CONCLUSIONS
....................................................
8
BIBLIOGRAPHY ..................................................
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MODEL STUDY OF PLASMAPAUSE MOTION
INTRODUCTION
A sharp drop in the ambient electron density with increasing altitude usually
occurs at a geocentric distance of a few earth radii near the equatorial plane
(Carpenter, 1963; Gringauz, 1963; Taylor et al., 1965). This region of abrupt
change is commonly referred to as the knee or as the plasmapause while the
high density region bounded by the plasmapause is called the plasma sphere.
The origin of the knee is best explained qualitatively by a model originally
developed by Nishida (1966). In this model, under steady state conditions the
knee is the boundary between plasma that drifts always across closed geomag-
netic field lines and plasma which at some time in its mot: )n drifts onto open
field lines (i.e., field lines which extend deep into the magnetospheric tail). In
the former plasma regime (the plasmasphere) plasma escape is always prevented
by closed field lines. Outside of the plasmasphere, however, a depletion of the
ambient plasma occurs due to escape along the open field lines into interplane-
tary space.
From whistler measurements (Figure 1) it is known that the knee position
in the equatorial plane is a function of local time with its maximum geocentric
distance usually occurring in the dusk sector. On the average, when the magnetic
.,:
index K
p
increases, the plasmapause moves to smaller L coordinates (Carpenter,
1966; Taylor et al., 1968; Binsack, 1967).
The time dependent motion of the plasmapause during magnetic substorms
is best characterized by the behavior of the bulge as deduced from ground based
k^
1

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Interplanetary Magnetic Field and the Auroral Zones

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A unifying theory of high-latitude geophysical phenomena and geomagnetic storms

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Whistler studies of the plasmapause in the magnetosphere: 1. Temporal variations in the position of the knee and some evidence on plasma motions near the knee

TL;DR: The position of the knee in the density of magnetospheric ionization was measured on a high time-resolution basis using whistlers recorded during July and part of August 1963 as discussed by the authors.
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Formation of plasmapause, or magnetospheric plasma knee, by the combined action of magnetospheric convection and plasma escape from the tail

TL;DR: In this article, the magnetic lines of force in the magnetosphere are separated into two groups: those that travel across the tail during the convective motion and those that are never transported to the tail.
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Coherence of geomagnetic DP 2 fluctuations with interplanetary magnetic variations

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