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Studying the Lunar Ionosphere with SELENE Radio Science Experiment
Authors:Takeshi Imamura  Takahiro Iwata  Zen-ichi Yamamoto  Nanako Mochizuki  Yusuke Kono  Koji Matsumoto  Qinghui Liu  Hirotomo Noda  Hideo Hanada  Koh-ichiro Oyama  Alexander Nabatov  Yoshifumi Futaana  Akinori Saito  Hiroki Ando
Institution:1. Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency, 3-1-1, Yoshinodai, Chuouku, Sagamihara, 252-5210, Japan
2. National Astronomical Observatory of Japan, National Institutes of Natural Sciences, 2-12 Hoshigaoka, Mizusawa, Oshu, 023-0861, Iwate, Japan
3. Shanghai Astronomical Observatory, Chinese Academy of Sciences, No. 80 Nandan Road, Shanghai, 200030, China
4. National Central University, 300, Jhongda Road, Jhongli, Taoyuan, 32001, Taiwan
5. Ukrainian Academy of Science, 4, Chervonoprapornaya Str., Kharkov, 61002, Ukraine
6. Swedish Institute of Space Physics, Box 812, 981 28, Kiruna, Sweden
7. Kyoto University, Gokasho, Uji City, Kyoto Prefecture, 611-0011, Japan
8. The University of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo, 113-0033, Japan
Abstract:Radio occultation observations of the electron density near the lunar surface were conducted during the SELENE (Kaguya) mission using the Vstar and Rstar sub-satellites. Previous radio occultation measurements conducted in the Soviet lunar missions have indicated the existence of an ionosphere with peak densities of several hundreds of electrons per cubic centimeters above the dayside lunar surface. These densities are difficult to explain theoretically when the removal of plasma by the solar wind is considered, and thus the generation mechanism of the lunar ionosphere is a major issue, with even the validity of previous observations still under debate. The most serious error source in the measurement is the fluctuation of the terrestrial ionosphere which also exists along the ray path. To cope with this difficulty, about 400 observations were conducted using Vstar to enable statistical analysis of the weak signal of the lunar ionosphere. Another method is to utilize Vstar and Rstar with the second one being used to measure the terrestrial ionosphere contribution. The observations will establish the morphology of the lunar ionosphere and will reveal its relationship with various conditions to provide possible clues to the mechanism.
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