The resolved layer of a collisionless, high β, supercritical, quasi-perpendicular shock wave: 1. Rankine-Hugoniot geometry, currents, and stationarity-Reference-Cited by-同舟云学术

The resolved layer of a collisionless, high β, supercritical, quasi-perpendicular shock wave: 1. Rankine-Hugoniot geometry, currents, and stationarity

Published:1986 Issue:A10 Volume:91 Page:11019
ISSN:0148-0227
Container-title:Journal of Geophysical Research
language:en
Short-container-title:J. Geophys. Res.

Author:

Scudder J. D.,Mangeney A.,Lacombe C.,Harvey C. C.,Aggson T. L.,Anderson R. R.,Gosling J. T.,Paschmann G.,Russell C. T.

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/v091/iA10/JA091iA10p11019/JA091iA10p11019.pdf

Reference60 articles.

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3. ISEE-1 and ISEE-2 fast plasma experiment and the ISEE-1 solar wind experiment;Bame;IEEE Trans. Geosci. Electron.,1978

4. High temporal resolution observations of electron heating;Bame;Space Sci. Rev.,1979

5. Collisionless shock waves in plasmas;Biskamp;Nucl. Fusion,1973

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