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凍土層を有する少雪寒冷地の融雪流出特性に関する研究
https://kitami-it.repo.nii.ac.jp/records/7402
https://kitami-it.repo.nii.ac.jp/records/7402a9f3f324-c8be-40fd-874c-fcc0c322c1de
名前 / ファイル | ライセンス | アクション |
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8663819-1.pdf (825.8 kB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2010-02-25 | |||||
タイトル | ||||||
言語 | ja | |||||
タイトル | 凍土層を有する少雪寒冷地の融雪流出特性に関する研究 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Study on Snowmelt Runoff Characteristics in the Cold and Snowy Region with Frozen Soil | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Snowmelt runoff | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | tank model | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | cold-content | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | frozen soil | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | degree hour method | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
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 | |||||
その他のタイトル | ||||||
その他のタイトル | Study on Snowmelt Runoff Characteristics in the Cold and Snowy Region with Frozen Soil | |||||
著者 |
早川, 博
× 早川, 博× 斎藤, 靖史× 内島, 邦秀 |
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著者別名 | ||||||
姓名 | Hayakawa, Hiroshi | |||||
言語 | en | |||||
著者別名 | ||||||
姓名 | Saito, Yasushi | |||||
言語 | en | |||||
著者別名 | ||||||
姓名 | Uchijima, Kunihide | |||||
言語 | en | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | This paper describes observations of snowmelt runoff with frozen soil in the Tomisato dam experimental basin. Observed results are indicated as follows: 1) the ground surface soil at the hillslopes was always freezing, 2) there was rarely frozen soil near the" stream channel because snowpack serves as a good thermal insulator, 3) the diurnal change of snowmelt runoff was rarely recognized except in the maximum snowmelt season and 4) the swell of long wavelength of hydrograph occurred in the early snowmelt season. To make clear the cause of above runoff characteristics, this study focuses on the overland flow over the hillslope surface and subsurface flow infiltrated in soil layers. By applying a 4X3 zoned tank model, it shows that the effects of frozen soil on the snowmelt runoff are estimated by the value of model parameters. | |||||
書誌情報 |
水工学論文集 巻 42, p. 127-132 |
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フォーマット | ||||||
内容記述タイプ | Other | |||||
内容記述 | application/pdf | |||||
出版者 | ||||||
出版者 | 社団法人 土木学会 | |||||
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 |