WEKO3
アイテム
魚野川上流域における融雪流出解析
http://hdl.handle.net/10649/412
http://hdl.handle.net/10649/412b3876b4e-3f02-4f99-9b61-1cac83f85231
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
K10_13.pdf (635.2 kB)
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| アイテムタイプ | 紀要論文 / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2011-02-15 | |||||
| タイトル | ||||||
| タイトル | 魚野川上流域における融雪流出解析 | |||||
| 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 | degree-day-factor method | |||||
| 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 | |||||
| 著者 |
樫村, 欣哉
× 樫村, 欣哉× 早川, 典生× 中村, 由行× 後藤, 巌 |
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| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 1720 | |||||
| 姓名 | カシムラ, キンヤ | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 1721 | |||||
| 姓名 | ハヤカワ, ノリオ | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 1722 | |||||
| 姓名 | ナカムラ, ヨシユキ | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 1723 | |||||
| 姓名 | ゴトウ, イワオ | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 1724 | |||||
| 姓名 | Kashimura, Kinya | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 1725 | |||||
| 姓名 | Hayakawa, Norio | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 1726 | |||||
| 姓名 | Nakamura, Yoshiyuki | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 1727 | |||||
| 姓名 | Gotou, Iwao | |||||
| 著者所属 | ||||||
| 値 | 株式会社鴻池組 | |||||
| 著者所属 | ||||||
| 値 | 長岡技術科学大学建設系 | |||||
| 著者所属 | ||||||
| 値 | 長岡技術科学大学建設系 | |||||
| 著者所属 | ||||||
| 値 | 長岡技術科学大学建設系 | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | The degree-day-factor (DDF) method is applied on the snowmelt runoff study for upper Uono River Basin with a catchment area of 335 km\^2^. The input data are daily precipitation at 3 rain gauging stations and temperature data at one station, whereas the output data are daily runoff of Uono River. Runoff model used is a lumped catchment model which takes into effect a variable source area. Procedure of runoff calculation is as follows. Precipitation data is split into rain and snow according to temperature data. Rain is to be fed into the runoff model, while snow accumulates itself to become snow cover. If temperature is above freezing, snowmelt runoff is generated according to the DDF method.There are two parameters in the snowmelt calculation, i.e. the degree-day-factor (DDF) and lapse rate of the temperature. The former in the snowmelt calculated runoff with the measured, while the latter is obtained from field temperature distribution. It was found that precipitation data during snowfall season has to be increased to obtain a good correspondence between calculated and measured runoff. This is also verified by referencing the calculated snowcover depth with snow depth survey data at nine stations. Furthermore a good correspondence is obtained by conjecturing snowfall increasing with elevation. | |||||
| 書誌情報 |
長岡技術科学大学研究報告 巻 10, p. 111-117, 発行日 1988-08 |
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| ISSN | ||||||
| 収録物識別子タイプ | ISSN | |||||
| 収録物識別子 | 0388-5631 | |||||
| 書誌レコードID | ||||||
| 収録物識別子タイプ | NCID | |||||
| 収録物識別子 | AN00177120 | |||||
| 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 | |||||
| その他のタイトル | ||||||
| その他のタイトル | Snowmelt runoff study for upper Uono river basin | |||||
| 出版者 | ||||||
| 出版者 | 長岡技術科学大学 | |||||
