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Venera‐9 magnetic field measurements in the Venus wake: Evidence for an Earth‐like interaction
Author(s) -
Russell C. T.
Publication year - 1976
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/gl003i008p00413
Subject(s) - venus , magnetosphere , geophysics , field (mathematics) , atmosphere of venus , plasma sheet , wake , physics , geology , mercury's magnetic field , magnetic field , astrobiology , earth's magnetic field , l shell , mechanics , quantum mechanics , mathematics , pure mathematics
Venera‐9 magnetic field measurements in the Venus wake provide additional support for the hypothesis that Venus has an intrinsic planetary field. The observed field is in the direction expected for a northward moment, and is similar to that observed in equivalent locations in the terrestrial magnetosphere, both in its temporal and spatial behavior. In particular, Venera‐9 appears to have observed a plasma sheet expansion, field‐aligned currents, and tail‐field dipolarization.

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