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嶮淵川におけるアイスジャムと河道狭窄の影響に関して
https://kitami-it.repo.nii.ac.jp/records/2000050
https://kitami-it.repo.nii.ac.jp/records/200005093629d82-cd5e-4a0f-8baa-28f4dfa449c4
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
河川技術論文集. 25, pp.91-96 (835 KB)
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| Item type | 学術雑誌論文 / Journal Article(1) | |||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 公開日 | 2021-05-26 | |||||||||||||
| タイトル | ||||||||||||||
| タイトル | 嶮淵川におけるアイスジャムと河道狭窄の影響に関して | |||||||||||||
| 言語 | ja | |||||||||||||
| タイトル | ||||||||||||||
| タイトル | INFLUENCE OF ICE JAM AND RIVER NARROWING IN KENUFUCHI RIVER | |||||||||||||
| 言語 | en | |||||||||||||
| 言語 | ||||||||||||||
| 言語 | jpn | |||||||||||||
| キーワード | ||||||||||||||
| 言語 | en | |||||||||||||
| 主題Scheme | Other | |||||||||||||
| 主題 | Ice jam | |||||||||||||
| キーワード | ||||||||||||||
| 言語 | en | |||||||||||||
| 主題Scheme | Other | |||||||||||||
| 主題 | Ice-covered river | |||||||||||||
| キーワード | ||||||||||||||
| 言語 | en | |||||||||||||
| 主題Scheme | Other | |||||||||||||
| 主題 | Numerical simulation | |||||||||||||
| 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 | journal article | |||||||||||||
| アクセス権 | ||||||||||||||
| アクセス権 | open access | |||||||||||||
| アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||||||||||
| 著者 |
伊波, 友生
× 伊波, 友生
× 横山, 洋× 吉川, 泰弘× 矢部, 浩規× 前田, 俊一
× 鳥谷部, 寿人 |
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| 抄録 | ||||||||||||||
| 内容記述タイプ | Abstract | |||||||||||||
| 内容記述 | On 9th March, 2018, due to unusual rainfall and temperature rise, ice jam occurred in the Kenufuchi River which has never been seen before. In the future, it is foreseen that water disaster will become more frequent with climate change, and rivers where ice jam occurs in Hokkaido will increase. However, ice jam has few observation cases, and its mechanism is not sufficiently elucidated. In order to clarify the occurrence factors of ice jam for the Kenufuchi River, the authors conducted a calculation of river ice variation. As a result, it was found that ice jam occurred due to increase in temperature and increase in discharge. Furthermore, river ice is easily formed because the flow velocity decreases in floor stop installed in the KP 7.1, and ice jam occurs meandering section. In consideration of the influence of river narrowing, it was found that river ice was formed thicker and the scale of ice jam increased. | |||||||||||||
| 言語 | en | |||||||||||||
| 書誌情報 |
ja : 河川技術論文集 巻 25, p. 91-96, 発行日 2019-06 |
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| 権利 | ||||||||||||||
| 権利情報 | c 2019 公益社団法人 土木学会 | |||||||||||||
| 出版者 | ||||||||||||||
| 出版者 | 土木学会 | |||||||||||||
| 言語 | ja | |||||||||||||
| 著者版フラグ | ||||||||||||||
| 値 | publisher | |||||||||||||
| 出版タイプ | ||||||||||||||
| 出版タイプ | VoR | |||||||||||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||||||||||
