Dipolarization fronts as a signature of transient reconnection in the magnetotail-Reference-Cited by-同舟云学术

Dipolarization fronts as a signature of transient reconnection in the magnetotail

Published:2009-04 Issue:A4 Volume:114 Page:n/a-n/a
ISSN:0148-0227
Container-title:Journal of Geophysical Research: Space Physics
language:en
Short-container-title:J. Geophys. Res.

Author:

Sitnov M. I.¹,Swisdak M.²,Divin A. V.³

Affiliation:

1. Applied Physics Laboratory; Johns Hopkins University; Laurel Maryland USA

2. Institute for Research in Electronics and Applied Physics; University of Maryland; College Park Maryland USA

3. Department of Mathematics; Katholieke Universiteit Leuven; Leuven Belgium

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference77 articles.

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4. Characteristics of high-speed ion flows in the plasma sheet;Baumjohann;J. Geophys. Res.,1990

5. Geospace Environmental Modeling (GEM) magnetic reconnection challenge;Birn;J. Geophys. Res.,2001

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