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高冷地における水の流出機構
http://hdl.handle.net/10091/2434
f0ac6d4c-a291-47f8-92c2-63409ebad643
名前 / ファイル | ライセンス | アクション | |
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2009-03-03 | |||||
タイトル | ||||||
タイトル | 高冷地における水の流出機構 | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
その他(別言語等)のタイトル | ||||||
その他のタイトル | Report on Runoff in the Cooler of High Elevation | |||||
著者 |
清水, 邦夫
× 清水, 邦夫 |
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出版者 | ||||||
出版者 | 信州大学農学部 | |||||
引用 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 信州大學紀要 8: 25-58(1958) | |||||
書誌情報 |
信州大學紀要 巻 8, p. 25-58, 発行日 1958-03-25 |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Runoff in the cooler region of high elevation is different from runoff in warm region of low elevation. (1) In the cooler region of high elevation we have not rain in winter and have snow, so heavy snow lies inside the area. In snowmelt-season, in spring, it runs off with rain or high-temperature and we have sometimes snowmelt-flood. (2) Generally we have more heavy rain in higher elevation, and in Nagano prefecture we have some areas where it rains more 5,000mm in a year. (3) Temperature influences runoff about 0℃, especially when surface of area freezes and runoff stops, base-flow becomes extremely lower. (4) Generally evaporation in the cooler region of high elevation is smaller. (5) From equation P=D+E+G+M P=precipitation D =discharge E=evaporation G=recharge of ground water through infiltration M=change of moisture we can cmpute monthly change of moisture, monthly moisture, daily change of moisture, and daily moisture. (6) We can compute that it is heavy rain in the foot of Mt. Komagatake, especially in 1956 it is 5406.3mm precipitation. We can compute that it is heavy snow in March 1956, so retention in area greatly increases. (7) Ground water level in the cooler region of high elevation, generally, is influenced by rain in warm and wet season, example June, and is not influenced by rain in winter so is lower. | |||||
資源タイプ(コンテンツの種類) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Article | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0583-0621 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00121068 |