Kinetic modeling of O+upflows resulting from E × B convection heating in the high-latitudeFregion ionosphere-Reference-Cited by-同舟云学术

Kinetic modeling of O+upflows resulting from E × B convection heating in the high-latitudeFregion ionosphere

Published:1994 Issue:A9 Volume:99 Page:17453
ISSN:0148-0227
Container-title:Journal of Geophysical Research
language:en
Short-container-title:J. Geophys. Res.

Author:

Wilson G. R.

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/v099/iA09/94JA01214/94JA01214.pdf

Reference34 articles.

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2. The ionospheric signatures of rapid subauroral ion drifts;Anderson;J. Geophys. Res.,1991

3. Banks, P. M., , G., Kockarts, , Aeronomy, Academic, San Diego, Calif., 1973,

4. O+ions in the polar wind;Barakat;J. Geophys. Res.,1983

5. Monte carlo calculations of the O+ velocity distribution in the auroral ionosphere;Barakat;J. Geophys. Res.,1983

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