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Whistler waves observed near lunar crustal magnetic sources
Author(s) -
Halekas J. S.,
Brain D. A.,
Mitchell D. L.,
Lin R. P.
Publication year - 2006
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 - 10.1029/2006gl027684
Subject(s) - whistler , physics , solar wind , geophysics , magnetic field , magnetometer , bow shock (aerodynamics) , mercury's magnetic field , shock wave , geology , interplanetary magnetic field , mechanics , quantum mechanics
We present Lunar Prospector Magnetometer (LP MAG) observations of monochromatic circularly polarized low frequency waves at frequencies of 0.4–4 Hz near the Moon. We observe such waves on about 6.6% of LP orbits in the solar wind, outside of the lunar wake. About a third of them occur on orbits when we also observe external magnetic enhancements (“limb shocks”), and most are clearly associated with lunar crustal magnetic sources, indicating an origin related to solar wind interaction with lunar magnetic fields. The inferred propagation vectors and polarizations of these waves are consistent with the expected characteristics of whistler‐mode waves. These observations could indicate either upstream whistler waves produced at shock surfaces above lunar crustal magnetic sources, or phase‐standing whistler wakes formed by direct solar wind interaction with lunar crustal magnetic fields.