[IGPP Everyone] TODAY: Space Physics Seminar, Fri. 3/17 3:30pm: "Oxygen Ions in Magnetotail Reconnection" (H. Liang, UCLA Physics)

Emmanuel V. Masongsong emasongsong at igpp.ucla.edu
Fri Mar 17 08:39:56 PDT 2017


SPACE PHYSICS SEMINAR 
DEPARTMENT OF EARTH, PLANETARY, AND SPACE SCIENCES 


DEPARTMENT OF ATMOSPHERIC AND OCEANIC SCIENCES 

UNIVERSITY OF CALIFORNIA, LOS ANGELES 



Oxygen Ions in Magnetotail Reconnection 



Haoming Liang 
UCLA Physics & Astronomy 



Spacecraft have observed a significant fraction of oxygen ions (O+) in Earth’s magnetotail X-line during the periods of enhanced geomagnetic activity. It is important to understand how such O+ influences the reconnection process and how the O+ ions are accelerated due to reconnection. To this end we have used a 2.5D implicit Particle-in-Cell simulation (iPIC3D) in a 2D Harris current sheet in the presence of proton and O+ ions. By comparing the simulation runs for oxygen concentrations of 50%, 5% and 0% (only protons), we found that (1) the dipolarization front (DF) propagation is encumbered by the current sheet O+ inertia, which reduces the DF speed and delays the fast reconnection phase; (2) the reconnection rate in the 50% O+ Run is much less than the 0% O+ Run, which can be attributed to the O+ drag on the convective magnetic flux via an ambipolar electric field in the O+ diffusion region; (3) without entering the exhaust, the lobe O+ can be accelerated near the separatrices away from the X-point by the Hall electric field and form the hot population downstream of the DFs; (4) the pre-existing current sheet O+ ions are reflected by the DFs and form a hook-shaped distribution in phase space, from which the DF speed history can be deduced; (5) the DF thickness is proportional to the O+ concentration in the pre-existing current sheet. These results illustrate the differences between storm-time and non-storm substorms due to a significant concentration of oxygen ions. The oxygen heating results are expected to be observable by the Magnetospheric Multiscale (MMS) mission in the magnetotail. 








Friday, March 17, 2016 

Room 6704 Geology 

3:30 - 5:00 PM 



In Charge 

V. Angelopoulos 




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