TY - JOUR
T1 - Night side lunar surface potential in the Earth's magnetosphere
AU - Saito, Y.
AU - Nishino, M. N.
AU - Yokota, S.
AU - Tsunakawa, H.
AU - Matsushima, M.
AU - Takahashi, F.
AU - Shibuya, H.
AU - Shimizu, H.
N1 - Funding Information:
The authors wish to express their sincere thanks to all the team members of MAP–PACE and MAP-LMAG for their great support in processing and analyzing the MAP data. The authors also wish to express their grateful thanks to all the system members of the SELENE project. This work was partly supported by JSPS Grant-in-Aid for Scientific Research (B) 21340143 .
PY - 2014/11/15
Y1 - 2014/11/15
N2 - In the Earth's magnetotail, Japanese Moon orbiter Kaguya repeatedly encountered the plasmoid or plasma sheet. The encounters were characterized by the low energy ion signatures including lobe cold ions, cold ion acceleration in the plasma sheet-lobe boundaries, and hot plasma sheet ions or fast flowing ions associated with plasmoids. Different from the previous observations made in the magnetotail by the GEOTAIL spacecraft, the ions were affected by the existence of the Moon. On the dayside of the Moon, tailward flowing cold ions and their acceleration were observed. However, on the night side, tailward flowing cold ions could not be observed since the Moon blocked them. In stead, ion acceleration by the spacecraft potential and the electron beam accelerated by the potential difference between lunar surface and spacecraft were simultaneously observed. These electron and ion data enabled us to determine the night side lunar surface potential and spacecraft potential only from the observed data for the first time.
AB - In the Earth's magnetotail, Japanese Moon orbiter Kaguya repeatedly encountered the plasmoid or plasma sheet. The encounters were characterized by the low energy ion signatures including lobe cold ions, cold ion acceleration in the plasma sheet-lobe boundaries, and hot plasma sheet ions or fast flowing ions associated with plasmoids. Different from the previous observations made in the magnetotail by the GEOTAIL spacecraft, the ions were affected by the existence of the Moon. On the dayside of the Moon, tailward flowing cold ions and their acceleration were observed. However, on the night side, tailward flowing cold ions could not be observed since the Moon blocked them. In stead, ion acceleration by the spacecraft potential and the electron beam accelerated by the potential difference between lunar surface and spacecraft were simultaneously observed. These electron and ion data enabled us to determine the night side lunar surface potential and spacecraft potential only from the observed data for the first time.
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U2 - 10.1016/j.asr.2013.05.011
DO - 10.1016/j.asr.2013.05.011
M3 - Article
AN - SCOPUS:84908223917
SN - 0273-1177
VL - 54
SP - 1985
EP - 1992
JO - Advances in Space Research
JF - Advances in Space Research
IS - 10
ER -