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中部山岳地域における融雪流出特性の標高依存性
http://hdl.handle.net/10091/17174
http://hdl.handle.net/10091/171745887a7b7-f155-4eb7-9677-77d099d8c960
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 | 2013-10-04 | |||||
タイトル | ||||||
言語 | ja | |||||
タイトル | 中部山岳地域における融雪流出特性の標高依存性 | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 融雪流出 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | snowmelt runoff | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 河川流量 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | river discharge | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 気候変動 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | climatic change | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 中部山岳地域 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Japanese Alps region | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 山岳水文 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | mountain hydrology | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | journal article | |||||
著者 |
山中, 勤
× 山中, 勤× 脇山, 義史× 鈴木, 啓助 |
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信州大学研究者総覧へのリンク | ||||||
氏名 | 鈴木, 啓助 | |||||
URL | http://soar-rd.shinshu-u.ac.jp/profile/ja.upTmOUkh.html | |||||
出版者 | ||||||
出版者 | 東京地学協会 | |||||
引用 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 地学雑誌. 122(4):682-693 (2013) | |||||
書誌情報 |
地学雑誌 巻 122, 号 4, p. 682-693, 発行日 2013 |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Observed discharge data covering the last three decades (1980-2009) at 16 rivers (i.e., rivers of Ida, Jinzu, Kurobe, Hime, Seki, Sai, Chikuma, Shinano, Uono, Kiso, Tenryu, Keta, Oi, Kamanashi, Fuefuki, and Fuji) in the Japanese Alps region are analyzed to clarify the elevation dependence of runoff characteristics during the snowmelt season. In the Hokuriku area, where large quantities of snow fall, the center time (CT) of snowmelt runoff tends to be delayed more at rivers with higher catchment-mean-elevations. In addition, the long-term (1980-2009) trend of a forward shift of snowmelt runoff timing becomes more remarkable at rivers in this area, with the exception of Hime River, as catchment-mean-elevation increases. However, the correlation between flowering dates of cherry trees and snowmelt runoff timing is stronger at rivers in the area with a lower catchment-mean-elevation. Consequently, snowmelt runoff at lower elevations in the Hokuriku area is sensitive to year-to-year fluctuations of spring onset, while progressive warming has greater impacts on snowmelt runoff timing at higher elevations, not only in winter to early spring but also in winter to late spring or summer. On the other hand, elevation dependence of snowmelt runoff timing is not detected at rivers in other areas; the runoff characteristics described above are neither clear nor statistically significant at both lower and higher elevations. Our results prove that the hydrological response to global warming is elevation dependent in a snow-dominated region, providing important knowledge for better water-resource management and flood control. | |||||
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 | 0022-135X | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00322536 | |||||
DOI | ||||||
識別子タイプ | DOI | |||||
関連識別子 | https://doi.org/10.5026/jgeography.122.682 | |||||
関連名称 | 10.5026/jgeography.122.682 | |||||
出版タイプ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |