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Landslide displacement detection around Hakusan volcano, central Japan, from InSAR analysis of ALOS-2/PALSAR-2 data
https://doi.org/10.24517/00051469
https://doi.org/10.24517/00051469d9f5b7bf-3ce4-4660-9546-800821ff3eac
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
Sci_Rep_61-39-47 (21.9 MB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2018-07-03 | |||||
| タイトル | ||||||
| タイトル | Landslide displacement detection around Hakusan volcano, central Japan, from InSAR analysis of ALOS-2/PALSAR-2 data | |||||
| 言語 | ||||||
| 言語 | eng | |||||
| キーワード | ||||||
| 言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | Interferometric synthetic aperture radar | |||||
| キーワード | ||||||
| 言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | Jinnosukedani area | |||||
| キーワード | ||||||
| 言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | Yunotani area | |||||
| キーワード | ||||||
| 言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | Sennindani area | |||||
| キーワード | ||||||
| 言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | Landslide movement | |||||
| キーワード | ||||||
| 言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | Slope collapse | |||||
| キーワード | ||||||
| 言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | GNSS observation | |||||
| 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 | 10.24517/00051469 | |||||
| ID登録タイプ | JaLC | |||||
| 著者 |
Kitoh, Yuya
× Kitoh, Yuya× Hiramatsu, Yoshihiro |
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| 著者別表示 |
平松, 良浩
× 平松, 良浩 |
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| 書誌情報 |
The Science Reports of Kanazawa University en : The Science Reports of Kanazawa University 巻 61, p. 39-47, 発行日 2017 |
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| ISSN | ||||||
| 収録物識別子タイプ | ISSN | |||||
| 収録物識別子 | 2433-040X | |||||
| 出版者 | ||||||
| 出版者 | Institute of Science and Engineering, Kanazawa University | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | nSAR analysis using ALOS-2/PALSAR-2 data was conducted to detect landslides around Hakusan volcano, where we observed landslide movements in three areas. In the Jinnosukedani area, we detected landslide movement with maximum annual displacement of 200 mm, which is consistent with that of GNSS observations on the ground surface. In the Yunotani area, we detected landslide movement with maximum annual displacement of 200 mm. The landslide area detected by the InSAR analysis is almost coincident with a previous study of InSAR analysis, although the remarkable landslide area with annual displacement of 100–200 mm is narrower than that reported by the previous study. In the Sennindani area, a large slope collapse can be captured by InSAR analysis as a low coherence area. InSAR analysis around Hakusan volcano provides results that are consistent with those of the ground-based monitoring in the field, indicating that InSAR analysis is a useful landslide-monitoring tool. | |||||
| 著者版フラグ | ||||||
| 出版タイプ | VoR | |||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
| 関連URI | ||||||
| 識別子タイプ | URI | |||||
| 関連識別子 | http://scirep.w3.kanazawa-u.ac.jp/ | |||||
