Tail lobe ion composition at energies of 0.1 to 16 keV/e: Evidence for mass-dependent density gradients

Author:

Lennartsson O. W.

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

Reference23 articles.

1. Magnetotail and boundary layer plasmas at a geocentric distance of ˜18RE: VELA 5 and 6 observations;Akasofu;J. Geophys. Res.,1973

2. Bevington, P. R., , Data Reduction and Error Analysis for the Physical Sciences, McGraw-Hill, New York, 1969,

3. Observations pertaining to the dynamics of the plasma sheet;DeCoster;J. Geophys. Res.,1979

4. A three-dimensional numerical model of ionospheric plasma in the magnetosphere;Delcourt;J. Geophys. Res.,1989

5. The boundary layers as the primary transport regions of the earth's magnetotail;Eastman;J. Geophys. Res.,1985

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