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ANALYSIS OF MOS-1 MSR DATA RECEIVED AT SYOWA STATION, ANTARCTICA
https://doi.org/10.15094/00003710
https://doi.org/10.15094/0000371038a910ae-a873-4ce4-9cad-2e75edf63b69
名前 / ファイル | ライセンス | アクション |
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KJ00002409939 (1.3 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1992-02-01 | |||||
タイトル | ||||||
タイトル | ANALYSIS OF MOS-1 MSR DATA RECEIVED AT SYOWA STATION, ANTARCTICA | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15094/00003710 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
論文名よみ | ||||||
その他のタイトル | ANALYSIS OF MOS-1 MSR DATA RECEIVED AT SYOWA STATION, ANTARCTICA | |||||
著者名よみ |
ヤマノウチ, タカシ
× ヤマノウチ, タカシ× オシヤマ, トモユキ× ワダ, マコト |
|||||
著者名(英) |
YAMANOUCHI, Takashi
× YAMANOUCHI, Takashi× OSHIYAMA, Tomoyuki× WADA, Makoto |
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著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
著者所属(英) | ||||||
en | ||||||
University of Electro-Communications:(Present address)Environmental Sciences, University of Tsukuba | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Atmospheric parameters and ground surface information are obtained using the MOS-1 MSR data received at Syowa Station, Antarctica. Several difficulties have appeared in the process of deriving water vapor amount and liquid water content. One is the antenna temperature, which includes large bias error; this causes the largest uncertainty. Also, the antenna temperature near the coast of the Antarctic continent was greatly affected by high brightness temperature of the ice sheet owing to the antenna side lobe, which caused difficulties in comparing with ground-based observations as a validation. In the normal condition, for the present example, water vapor amount ranged from 0.4 to 1.4g/(cm)^2 and liquid water contentfrom 0 to 14mg/(cm)^2. However, there was found a belt of high liquid water content in some paths, corresponding to a high brightness temperature of about 190K. The atmospheric water vapor or liquid water affects the estimation of surface conditions such as sea ice concentration. It is difficult to obtain atmospheric parameters over the ice sheet and sea ice, on account of their high and variable brightness temperature. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA10756213 | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology 巻 5, p. 156-166, 発行日 1992-02 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |