Oxygen torus in the deep inner magnetosphere and its contribution to recurrent process of O+-rich ring current formation-Reference-Cited by-同舟云学术

Oxygen torus in the deep inner magnetosphere and its contribution to recurrent process of O+-rich ring current formation

Published:2011-10 Issue:A10 Volume:116 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:

Nosé M.¹,Takahashi K.²,Anderson R. R.³,Singer H. J.⁴

Affiliation:

1. Data Analysis Center for Geomagnetism and Space Magnetism, Graduate School of Science; Kyoto University; Kyoto Japan

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

3. Department of Physics and Astronomy; University of Iowa; Iowa City Iowa USA

4. Space Weather Prediction Center, National Centers for Environmental Prediction; NOAA/National Weather Service; Boulder Colorado USA

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

Link

http://www.agu.org/journals/ja/ja1110/2011JA016651/2011JA016651.pdf

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3. An ISEE/whistler model of equatorial electron density in the magnetosphere;Carpenter;J. Geophys. Res.,1992

4. Initial observations of thermal plasma composition and energetics from Dynamics Explorer-1;Chappell;Geophys. Res. Lett.,1982

5. A study of the influence of magnetic activity on the location of the plasmapause as measured by OGO 5;Chappell;J. Geophys. Res.,1970

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