First direct detection of ions originating from the Moon by MAP‐PACE IMA onboard SELENE (KAGUYA)

  • Shoichiro Yokota
    Institute of Space and Astronautical Science Japan Aerospace Exploration Agency Sagamihara Japan
  • Yoshifumi Saito
    Institute of Space and Astronautical Science Japan Aerospace Exploration Agency Sagamihara Japan
  • Kazushi Asamura
    Institute of Space and Astronautical Science Japan Aerospace Exploration Agency Sagamihara Japan
  • Takaaki Tanaka
    Institute of Space and Astronautical Science Japan Aerospace Exploration Agency Sagamihara Japan
  • Masaki N. Nishino
    Institute of Space and Astronautical Science Japan Aerospace Exploration Agency Sagamihara Japan
  • Hideo Tsunakawa
    Department of Earth and Planetary Sciences Tokyo Institute of Technology Tokyo Japan
  • Hidetoshi Shibuya
    Department of Earth Science Kumamoto University Kumamoto Japan
  • Masaki Matsushima
    Department of Earth and Planetary Science University of Tokyo Tokyo Japan
  • Hisayoshi Shimizu
    Earthquake Research Institute University of Tokyo Tokyo Japan
  • Futoshi Takahashi
    Department of Earth and Planetary Sciences Tokyo Institute of Technology Tokyo Japan
  • Masaki Fujimoto
    Institute of Space and Astronautical Science Japan Aerospace Exploration Agency Sagamihara Japan
  • Toshifumi Mukai
    Institute of Space and Astronautical Science Japan Aerospace Exploration Agency Sagamihara Japan
  • Toshio Terasawa
    Department of Physics Tokyo Institute of Technology Tokyo Japan

書誌事項

公開日
2009-06
権利情報
  • http://onlinelibrary.wiley.com/termsAndConditions#vor
DOI
  • 10.1029/2009gl038185
公開者
American Geophysical Union (AGU)

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説明

<jats:p>The Moon has no global intrinsic magnetic field and only has a very thin atmosphere. Ion measurements made from lunar orbit provide us with information regarding interactions between the solar wind and planetary surface, the surface composition through secondary ion mass spectrometry and the source and loss mechanisms of planetary tenuous atmosphere. An ion energy mass spectrometer MAP‐PACE IMA onboard a lunar orbiter SELENE (KAGUYA) has detected low‐energy ions at 100‐km altitude. The MAP‐PACE measurements have elucidated that the ions originate from the lunar surface and exosphere and that the ions are at least composed of He<jats:sup>+</jats:sup>, C<jats:sup>+</jats:sup>, O<jats:sup>+</jats:sup>, Na<jats:sup>+</jats:sup> and K<jats:sup>+</jats:sup>. Following the discovery of the lunar Na and K exospheres by the ground‐based observation, MAP‐PACE IMA have found the He, C and O exospheres around the Moon.</jats:p>

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