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APPLICABILITY OF 10Hz SATELLITE ALTIMETRY DATA TO THE ANTARCTIC MARGIN
https://doi.org/10.15094/00002841
https://doi.org/10.15094/0000284107a95540-486e-471a-be7c-66eb1d672556
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00002368114 (1.4 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1997-09-01 | |||||
タイトル | ||||||
タイトル | APPLICABILITY OF 10Hz SATELLITE ALTIMETRY DATA TO THE ANTARCTIC MARGIN | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | altimetry | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | gravity | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Geosat/GM | |||||
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 | 10.15094/00002841 | |||||
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 | APPLICABILITY OF 10Hz SATELLITE ALTIMETRY DATA TO THE ANTARCTIC MARGIN | |||||
著者名よみ |
テラダ, クミコ
× テラダ, クミコ× フクダ, ヨウイチ |
|||||
著者名(英) |
TERADA, Kumiko
× TERADA, Kumiko× FUKUDA, Yoichi |
|||||
著者所属(英) | ||||||
en | ||||||
Graduate School of Science, Kyoto University | ||||||
著者所属(英) | ||||||
en | ||||||
Graduate School of Science, Kyoto University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Since the declassification of the Geosat Geodetic Mission (Geosat/GM), cross-track resolution of satellite altimeter profiles has improved remarkably. Consequently, the cross-track resolution somewhat exceeds the along-track resolution. To utilize the high-density of Geosat/GM profiles, we examine whether the along-track resolution is improved by using the 10Hz sampling data or not. For this purpose, Geosat/GM profiles in the Southern Ocean and Antarctic margin are mainly tested. Ten Hz data are converted into grids of gravity anomaly following the recipe given by D.T. SANDWELL (Geophys. J. Int., 109,437,1992). The converted grids are then compared with the grids of high-cut filtered data. The result implies that the 10 Hz data can show more detailed structures than filtered data. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1072335X | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Antarctic Geosciences 巻 10, p. 26-35, 発行日 1997-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |