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少雪寒冷地における凍結土層の存在を考慮した融雪流出モデルに関する研究
https://kitami-it.repo.nii.ac.jp/records/7403
https://kitami-it.repo.nii.ac.jp/records/740379316728-7d9a-425f-abdc-db405c37c2d9
名前 / ファイル | ライセンス | アクション |
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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 | 少雪寒冷地における凍結土層の存在を考慮した融雪流出モデルに関する研究 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Study on Snowmelt Runoff Model 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 | frozen soil | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | freezing index | |||||
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 Model in the Cold and Snowy Region with Frozen Soil | |||||
著者 |
早川, 博
× 早川, 博× 松本, 隆志× 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 | MATSUMOTO, Takashi | |||||
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 | In Hokkaido, we have often experienced ground surface freezing during the winter. The Tomisato dam experiment basin was set up to clarify the effects of frozen soil on the snowmelt runoff. It is possible in snowmelt season to occur the overland flow at the hillslopes because of reducing infiltration capacity of ground surface by soil freezing. By analyzing observed data, it was pointed out that the swell of long wavelength of hydrograph occurred in the early snowmelt season. To make clear the effects of frozen soil on the snowmelt runoff, we reconstruct 4 X 3 zoned tank model, which can consider the spatially distributed frost depth and snow depth at this site, by including the frost dept prediction model. By multiple regression analysis, the frost depth is good relationship between freezing index, snow depth and melting index, and the max value of frost depth is dependent upon the accumulate rainfall at autumn season. As a result, it shows that this improvement is effective to estimate the snowmelt runoff in | |||||
書誌情報 |
水工学論文集 巻 45, p. 67-72 |
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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 |