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北アルプスにおける冬季降水中の化学成分濃度
http://hdl.handle.net/10091/17183
76cb113a-c76f-4894-a561-c8fd494e3fba
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 | en | |||||
タイトル | Winter precipitation chemistry at a high elevation site of Japan Northern Alps | |||||
タイトル | ||||||
言語 | ja | |||||
タイトル | 北アルプスにおける冬季降水中の化学成分濃度 | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | an Northern Alps | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 北アルプス | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | winter precipitation | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 冬季降水 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | chemical constituents | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 化学成分 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | mountain barrier | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 山岳地形 | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | journal article | |||||
著者 |
田中, 基樹
× 田中, 基樹× 鈴木, 啓助 |
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信州大学研究者総覧へのリンク | ||||||
氏名 | SUZUKl, Keisuke | |||||
URL | http://soar-rd.shinshu-u.ac.jp/profile/ja.upTmOUkh.html | |||||
出版者 | ||||||
出版者 | Japanese Society of Snow and Ice | |||||
引用 | ||||||
内容記述タイプ | Other | |||||
内容記述 | Bulletin of Glaciological Research. 28:17-26 (2010) | |||||
書誌情報 |
Bulletin of Glaciological Research 巻 28, p. 17-26, 発行日 2010 |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Spatial variability of the chemical constituents of winter precipitation on the eastern-western slopes of Mt. Norikura (alt. 3025m) of Japan Northern Alps was examined to clarify the transport process of aerosol that flows over the mountain barrier. The concentrations of chemical constituents in the snow recorded at the upper part of the mountain (above alt. 2420m) make a little difference. However, at the lower part of the mountain (below alt. 2420m), Cl- concentration in the snow on the eastern slope was lower than that on the western slope; non-sea-salt SO42- (nssSO42-), NO3-, nssCa2+, nssMg2+ and NH4+ concentrations on the eastern slope was higher than that on the western slope. The prevailing westerlies raged at the western and alpine parts of the mountain. On the eastern part of the mountain, the easterlies were predominant. We infer that the snow below an altitude of 2420m, in comparison to the other parts of mountain, is under relatively greater influence of the local emission of the chemical constituents. | |||||
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 | PISSN | |||||
収録物識別子 | 1345-3807 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA11582242 | |||||
DOI | ||||||
関連タイプ | isIdenticalTo | |||||
関連識別子 | ||||||
識別子タイプ | DOI | |||||
関連識別子 | https://doi.org/10.5331/bgr.28.17 | |||||
関連名称 | ||||||
関連名称 | 10.5331/bgr.28.17 | |||||
権利 | ||||||
権利情報 | © 2010 Japanese Society of Snow and Ice | |||||
出版タイプ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |