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Statistical characterization of the foremoon particle and wave morphology: ARTEMIS observations
Journal article   Open access   Peer reviewed

Statistical characterization of the foremoon particle and wave morphology: ARTEMIS observations

Y Harada, J. S Halekas, A. R Poppe, Y Tsugawa, S Kurita and J. P McFadden
Journal of geophysical research. Space physics, Vol.120(6), pp.4907-4921
06/2015
DOI: 10.1002/2015JA021211
url
https://doi.org/10.1002/2015JA021211View
Published (Version of record) Open Access

Abstract

Although the zeroth-order picture of the Moon-solar wind interaction involves no upstream perturbation, the presence of the Moon does affect the upstream plasma in a variety of ways. In this paper, a large volume of data obtained by the dual-probe Acceleration, Reconnection, Turbulence and Electrodynamics of the Moon's Interaction with the Sun (ARTEMIS) mission are used to characterize the large-scale morphology of the "foremoon," which is defined as the region upstream of the Moon and its wake that contains Moon-related particles and waves. Solar wind ions reflected from the unshielded surface and by crustal magnetic fields, together with heavy ions of lunar surface/exospheric origin, are picked up by the solar wind magnetic and electric fields. Partially coinciding with populations of these Moon-related ions, ∼0.01 Hz and ∼1 Hz magnetic field fluctuations are observed. The morphology of the Moon-related ion and wave distributions is well organized by the upstream magnetic field direction. In addition, the low-frequency wave distributions depend on the upstream Alfvén Mach numbers, suggesting that propagation effects also play a role in determining the wave foremoon morphology. Occurrence of modified electron velocity distributions and higher-frequency, electromagnetic, and electrostatic waves is primarily controlled by magnetic connection to the Moon and its wake. These statistical results observationally demonstrate the large-scale properties of the foremoon and upstream-parameter control thereof. Key Points ARTEMIS observes a wide variety of lunar upstream particles and waves Global distributions of lunar upstream phenomena are organized by IMF direction Low-frequency wave distributions are controlled by Mach numbers

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