In-flight Performance and Initial Results of Plasma Energy Angle and Composition Experiment (PACE) onSELENE (Kaguya)
MAP-PACE (MAgnetic field and Plasma experiment--Plasma energy Angle and Composition Experiment) on SELENE (Kaguya) has completed its 1.5-year observation of low-energy charged particles around the Moon. MAP-PACE consists of 4 sensors: ESA (Electron Spectrum Analyzer)-S1, ESA-S2, IMA (Ion Mass Analyz...
Gespeichert in:
Veröffentlicht in: | Space science reviews 2010-07, Vol.154 (1-4), p.265-303 |
---|---|
Hauptverfasser: | , , , , , , , , , , , , , , , , , , , , , , , , , , , , |
Format: | Artikel |
Sprache: | eng |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
Zusammenfassung: | MAP-PACE (MAgnetic field and Plasma experiment--Plasma energy Angle and Composition Experiment) on SELENE (Kaguya) has completed its 1.5-year observation of low-energy charged particles around the Moon. MAP-PACE consists of 4 sensors: ESA (Electron Spectrum Analyzer)-S1, ESA-S2, IMA (Ion Mass Analyzer), and IEA (Ion Energy Analyzer). ESA-S1 and S2 measured the distribution function of low-energy electrons in the energy range 6 eV-9 keV and 9 eV-16 keV, respectively. IMA and IEA measured the distribution function of low-energy ions in the energy ranges 7 eV/q-28 keV/q and 7 eV/q-29 keV/q. All the sensors performed quite well as expected from the laboratory experiment carried out before launch. Since each sensor has a hemispherical field of view, two electron sensors and two ion sensors installed on the spacecraft panels opposite each other could cover the full 3-dimensional phase space of low-energy electrons and ions. One of the ion sensors IMA is an energy mass spectrometer. IMA measured mass-specific ion energy spectra that have never before been obtained at a 100 km altitude polar orbit around the Moon. The newly observed data show characteristic ion populations around the Moon. Besides the solar wind, MAP-PACE-IMA found four clearly distinguishable ion populations on the dayside of the Moon: (1)Solar wind protons backscattered at the lunar surface, (2)Solar wind protons reflected by magnetic anomalies on the lunar surface, (3)Reflected/backscattered protons picked-up by the solar wind, and (4)Ions originating from the lunar surface/lunar exosphere. |
---|---|
ISSN: | 0038-6308 1572-9672 |
DOI: | 10.1007/s11214-010-9647-x |