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  1. 040 理学部
  2. 0401 学術論文

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/10091/17174
5887a7b7-f155-4eb7-9677-77d099d8c960
名前 / ファイル ライセンス アクション
Chigaku_Zasshi_122_4_682.pdf Chigaku_Zasshi_122_4_682.pdf (1.3 MB)
Item type 学術雑誌論文 / Journal Article(1)
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

WEKO 36067

山中, 勤

Search repository
脇山, 義史

× 脇山, 義史

WEKO 36068

脇山, 義史

Search repository
鈴木, 啓助

× 鈴木, 啓助

WEKO 36069

鈴木, 啓助

Search repository
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
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
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