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  1. 070 農学部, 大学院農学研究科
  2. 0702 紀要 ・刊行物
  3. 07023 信州大學紀要. 第五輯, 農學部
  4. No. 8

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
Agriculture08-02.pdf Agriculture08-02.pdf (1.4 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
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

WEKO 34882

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
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
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