Evidence for >30-keV Electrons Accelerated in the Shock Transition Region Beyond the Earth's Magnetospheric Boundary

1964 ◽  
Vol 13 (5) ◽  
pp. 149-152 ◽  
Author(s):  
C. Y. Fan ◽  
G. Gloeckler ◽  
J. A. Simpson
Keyword(s):  
Transition Region ◽  
Magnetospheric Boundary ◽  
Shock Transition

The dynamics of electron–ion coupling in the shock transition region

2003 ◽  
Vol 10 (4) ◽  
pp. 1113-1119 ◽  
Author(s):  
Nobue Shimada ◽  
Masahiro Hoshino
Keyword(s):  
Transition Region ◽  
Shock Transition

scholarly journals Bipolar electrostatic structures in the shock transition region: Evidence of electron phase space holes

1998 ◽  
Vol 25 (15) ◽  
pp. 2929-2932 ◽  
Author(s):  
S. D. Bale ◽  
P. J. Kellogg ◽  
D. E. Larsen ◽  
R. P. Lin ◽  
K. Goetz ◽  
...  
Keyword(s):  
Phase Space ◽  
Transition Region ◽  
Shock Transition

scholarly journals Observational Evidence of Magnetic Reconnection in the Terrestrial Bow Shock Transition Region

2019 ◽  
Vol 46 (2) ◽  
pp. 562-570 ◽  
Author(s):  
Shan Wang ◽  
Li‐Jen Chen ◽  
Naoki Bessho ◽  
Michael Hesse ◽  
Lynn B. Wilson ◽  
...  
Keyword(s):  
Magnetic Reconnection ◽  
Transition Region ◽  
Observational Evidence ◽  
Bow Shock ◽  
Shock Transition

Effects of Ambipolar Diffusion on Prominence Thread Models

1994 ◽  
Vol 144 ◽  
pp. 315-321 ◽  
Author(s):  
M. G. Rovira ◽  
J. M. Fontenla ◽  
J.-C. Vial ◽  
P. Gouttebroze
Keyword(s):  
Energy Balance ◽  
Transition Region ◽  
Ambipolar Diffusion ◽  
Line Profiles ◽  
Balance Equations ◽  
Model Calculations ◽  
Partial Frequency ◽  
Frequency Redistribution ◽  
Partial Frequency Redistribution ◽  
Theoretical Structure

AbstractWe have improved previous model calculations of the prominence-corona transition region including the effect of the ambipolar diffusion in the statistical equilibrium and energy balance equations. We show its influence on the different parameters that characterize the resulting prominence theoretical structure. We take into account the effect of the partial frequency redistribution (PRD) in the line profiles and total intensities calculations.

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