Substorm activity on January 11, 1994: Geotail observations in the distant tail during the leading phase of a corotating interaction region

Author:

Wilken B.,Zong Q.-G.,Doke T.,Mukai T.,Yamamoto T.,Reeves G. D.,Maezawa K.,Kokubun S.,Ullaland S.

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

Reference42 articles.

1. A possible interpretation of cold ion beams in the earth's tail lobe;Baker;J. Geomagn. Geoelectr.,1996

2. Solar wind heavy ion abundances;Bame;Sol. Phys.,1975

3. Evidence for interplanetary acceleration of nucleons in corotating interaction regions;Barnes;Astrophys. J. Lett.,1976

4. Helium abundance enhancements in the solar wind;Borrini;J. Geophys. Res.,1982

5. Energetic atomic and molecular ions of ionospheric origin observed in distant magnetotail flow-reversal events;Christon;Geophys. Res. Lett.,1994

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1. ISAS-NASA GEOTAIL Satellite (1992);Handbook of Cosmic Hazards and Planetary Defense;2015

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3. Statistical study of the properties of the magnetic field and plasma in the earth’s magnetotail near lunar orbit;Science China Technological Sciences;2012-07-20

4. Substorm-like magnetospheric response to a discontinuity in the Bxcomponent of interplanetary magnetic field;Journal of Geophysical Research: Space Physics;2012-04

5. Shrinkage of magnetosphere observed by TC-1 satellite during the high-speed solar wind stream;Science in China Series E: Technological Sciences;2008-09-14

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