The magnetosphere of Venus: Evidence for a boundary layer and a magnetotail
- 1 October 1976
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 3 (10) , 589-592
- https://doi.org/10.1029/gl003i010p00589
Abstract
A detailed examination of Mariner 5 magnetic field data reveals evidence for a boundary layer beginning in the dayside ionosphere, and a magnetotail much like the terrestrial magnetotail in accord with Venera measurements.This publication has 9 references indexed in Scilit:
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- The magnetic moment of Venus: Venera‐4 measurements reinterpretedGeophysical Research Letters, 1976
- Heos 2 plasma observations in the distant polar magnetosphere: The plasma mantleJournal of Geophysical Research, 1975
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- Magnetotail and boundary layer plasmas at a geocentric distance of ∼18RE: Vela 5 and 6 observationsJournal of Geophysical Research, 1973
- Speed and thickness of the magnetopauseJournal of Geophysical Research, 1973
- Solar wind flow past nonmagnetic planets—Venus and MarsPlanetary and Space Science, 1970
- Modification of the Martian ionosphere by the solar windJournal of Geophysical Research, 1969
- Mariner V: Plasma and Magnetic Fields Observed near VenusScience, 1967