The source of O+ in the storm time ring current-Reference-Cited by-同舟云学术

The source of O+ in the storm time ring current

Published:2016-06 Issue:6 Volume:121 Page:5333-5349
ISSN:2169-9380
Container-title:Journal of Geophysical Research: Space Physics
language:en
Short-container-title:J. Geophys. Res. Space Physics

Author:

Kistler L. M.¹,Mouikis C. G.¹,Spence H. E.¹,Menz A. M.¹,Skoug R. M.²,Funsten H. O.²,Larsen B. A.²,Mitchell D. G.³,Gkioulidou M.³,Wygant J. R.⁴,Lanzerotti L. J.⁵

Affiliation:

1. Space Science Center; University of New Hampshire; Durham New Hampshire USA

2. Los Alamos National Laboratory; Los Alamos New Mexico USA

3. The Johns Hopkins University Applied Physics Laboratory; Laurel Maryland USA

4. School of Physics and Astronomy; University of Minnesota; Minneapolis Minnesota USA

5. Center for Solar-Terrestrial Research; New Jersey Institute of Technology; Newark New Jersey USA

Funder

NASA

RBSP-ECT

JHU/APL

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2015JA022204/fullpdf

Reference31 articles.

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2. Observations of the warm plasma cloak and an explanation of its formation in the magnetosphere;Chappell;J. Geophys. Res.,2008

3. Extreme ionospheric ion energization and electron heating in Alfvén waves in the storm time inner magnetosphere;Chaston;Geophys. Res. Lett.,2015

4. Supply of thermal ionospheric ions to the central plasma sheet;Cully;J. Geophys. Res.,2003

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