scholarly journals Validation of Anisotropic Electron Fluid Closure Through In Situ Spacecraft Observations of Magnetic Reconnection

2019 ◽  
Vol 46 (12) ◽  
pp. 6223-6229
Author(s):  
Blake A. Wetherton ◽  
Jan Egedal ◽  
Ari Lê ◽  
William Daughton
2014 ◽  
Vol 119 (12) ◽  
pp. 9952-9961 ◽  
Author(s):  
Rongsheng Wang ◽  
Quanming Lu ◽  
Aimin Du ◽  
Rumi Nakamura ◽  
San Lu ◽  
...  

2020 ◽  
Vol 246 (2) ◽  
pp. 34 ◽  
Author(s):  
T. D. Phan ◽  
S. D. Bale ◽  
J. P. Eastwood ◽  
B. Lavraud ◽  
J. F. Drake ◽  
...  

2007 ◽  
Vol 3 (4) ◽  
pp. 235-238 ◽  
Author(s):  
A. Retinò ◽  
D. Sundkvist ◽  
A. Vaivads ◽  
F. Mozer ◽  
M. André ◽  
...  

2013 ◽  
Vol 8 (S300) ◽  
pp. 502-503
Author(s):  
L. van Driel-Gesztelyi ◽  
D. Baker ◽  
T. Török ◽  
E. Pariat ◽  
L. M. Green ◽  
...  

AbstractDuring an unusually massive filament eruption on 7 June 2011, SDO/AIA imaged for the first time significant EUV emission around a magnetic reconnection region in the solar corona. The reconnection occurred between magnetic fields of the laterally expanding CME and a neighbouring active region. A pre-existing quasi-separatrix layer was activated in the process. This scenario is supported by data-constrained numerical simulations of the eruption. Observations show that dense cool filament plasma was re-directed and heated in situ, producing coronal-temperature emission around the reconnection region. These results provide the first direct observational evidence, supported by MHD simulations and magnetic modelling, that a large-scale re-configuration of the coronal magnetic field takes place during solar eruptions via the process of magnetic reconnection.


2005 ◽  
Vol 23 (8) ◽  
pp. 2903-2907 ◽  
Author(s):  
J. A. Wild ◽  
S. E. Milan ◽  
J. A. Davies ◽  
S. W. H. Cowley ◽  
C. M. Carr ◽  
...  

Abstract. We present a space- and ground-based study exploiting data from the coordinated Cluster and Double Star missions in order to investigate dayside magnetic reconnection under BY+ dominated IMF conditions. In-situ observations of magnetosheath flux transfer events combined with measurements of pulsed poleward and dawnward directed flows in the pre-noon sector high-latitude northern hemisphere ionosphere are interpreted as indications of pulsed magnetic reconnection during an interval in which the IMF remained relatively steady. Observations of newly-reconnected magnetic flux tubes anchored in the northern hemisphere both at mid-latitudes and in the vicinity of the subsolar point suggests that during BY+ dominated IMF, reconnection is not, as proposed previously, limited to the high-latitude magnetopause.


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