Interplanetary magnetic holes: Theory
- 1 November 1978
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 83 (A11) , 5157-5160
- https://doi.org/10.1029/ja083ia11p05157
Abstract
Magnetic holes in the interplanetary medium are explained as stationary nonpropagating equilibrium structures in which there are field‐aligned enhancements of the plasma density and/or temperature. Magnetic antiholes are considered to be associated with depressions in the plasma pressure. In this model the observed changes in the magnetic field intensity and direction are due to diamagnetic currents that are carried by ions which drift in a sheath as the result of gradients in the magnetic field and in the plasma pressure within the sheath. The thickness of the sheaths that we consider is approximately a few ion Larmor radii. An electric field is normal to the magnetic field in the sheath. Solutions of Vlasov's equation and Maxwell's equations are presented which account for several types of magnetic holes, including ‘null sheets,’ that have been observed.Keywords
This publication has 5 references indexed in Scilit:
- Structure of current sheets in magnetic holes at 1 AUJournal of Geophysical Research, 1978
- Magnetic holes in the solar windJournal of Geophysical Research, 1977
- Diamagnetic boundary layers: A kinetic theoryAstrophysics and Space Science, 1976
- The Microstructure of the MagnetopauseGeophysical Journal International, 1975
- Structure of the magnetopauseReviews of Geophysics, 1971