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Polar caps of Mars: Snow depth data and Viking pressure curves
https://jaxa.repo.nii.ac.jp/records/20666
https://jaxa.repo.nii.ac.jp/records/20666fd835883-1635-41dd-ad96-090ba600e12a
Item type | 会議発表論文 / Conference Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 2015-03-26 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Polar caps of Mars: Snow depth data and Viking pressure curves | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | MGS | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 火星 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 極冠 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 雪深度 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 年変動 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 2酸化炭素 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | MOLA | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Viking圧力曲線 | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | MGS | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Mars | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | polar cap | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | snow depth | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | annual variation | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | carbon dioxide | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | MOLA | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Viking pressure curve | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_5794 | |||||
資源タイプ | conference paper | |||||
アクセス権 | ||||||
アクセス権 | metadata only access | |||||
アクセス権URI | http://purl.org/coar/access_right/c_14cb | |||||
その他のタイトル | ||||||
その他のタイトル | 火星極冠:雪深度データおよびViking圧力曲線 | |||||
著者 |
鳴海, 泰典
× 鳴海, 泰典× Narumi, Yasunori |
|||||
著者所属 | ||||||
九州東海大学 | ||||||
著者所属(英) | ||||||
en | ||||||
Kyushu Tokai University | ||||||
出版者 | ||||||
出版者 | 宇宙航空研究開発機構宇宙科学研究本部 | |||||
出版者(英) | ||||||
出版者 | Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency (JAXA/ISAS) | |||||
書誌情報 |
第36回月・惑星シンポジウム en : Proceedings of the 36th ISAS Lunar and Planetary Symposium p. 65-68, 発行日 2003-11 |
|||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Smith et al. (2001) reported the seasonal variations of snow depth on Mars using topography collected from the Mars Orbiter Laser Altimeter (MOLA) on the Mars Global Surveyor (MGS). A seasonal pressure variation curve was derived from the snow depth data of Smith et al. (2001), and it was compared with the Viking pressure curves. The agreement of those two pressure variation curves is not so good. At first, the amplitude of seasonal pressure variation derived from the snow depth data is smaller than that of Viking observations. This means that the CO2 ice amount accumulated on polar regions during winter season was not so large as expected by the Viking pressure variation curves. Next, the phase of minimum and maximum pressure differs in those two pressure curves. For example, in the pressure curve derived from the snow depth data, the maximum pressure occurs a little earlier than that in the Viking pressure curves. This suggests that the CO2 ice evaporation in the south hemisphere during the snow depth observation may be earlier than that during the Viking observations. Finally, the snow depth data show the large effect of dust storms. On the other hand, the Viking Lander data show little effect of dust storms. There is a possibility that the meteorological environment of Mars suffered some variations since the time of the Viking observations. | |||||
資料番号 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 資料番号: AA0046650017 |