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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降雪条件の違いによる積雪中の化学特性

http://hdl.handle.net/10091/17182
7a8adb30-da87-4485-bef4-8553763b1ef1
名前 / ファイル ライセンス アクション
BGR26P15-Kuramoto_et_al.pdf BGR26P15-Kuramoto_et_al.pdf (731.3 kB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2013-10-04
タイトル
言語 en
タイトル Chemical Characteristics of Snowpack due to Differences in Snowfall Type in Japan Alps
タイトル
言語 ja
タイトル 中部山岳地域における降雪条件の違いによる積雪中の化学特性
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ journal article
著者 倉元, 隆之

× 倉元, 隆之

WEKO 36044

en KURAMOTO, Takayuki

ja 倉元, 隆之

Search repository
SHAH, Shailendra Kumar

× SHAH, Shailendra Kumar

WEKO 36045

en SHAH, Shailendra Kumar

Search repository
田中, 基樹

× 田中, 基樹

WEKO 36046

en TANAKA, Motoki

ja 田中, 基樹

Search repository
鈴木, 啓助

× 鈴木, 啓助

WEKO 36047

en SUZUKl, Keisuke

ja 鈴木, 啓助

Search repository
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. 26:15-21 (2008)
書誌情報 Bulletin of Glaciological Research

巻 26, p. 15-21, 発行日 2008
抄録
内容記述タイプ Abstract
内容記述 We conducted a snow survey in February 2006 and January 2007 in Japan Alps. Approximately 0.60m and 1.05m snowfalls were deposited at the study site in February 2006 and January 2007, respectively. It was observed that the occurrence of snowfall was due to the low pressure formation in the vicinity of Japan and it also being the winter monsoon period. As a result of the analyzed snowpack, including new snow at a high resolution every 0.03m, a plurality of high-electric conductivity layers were observed at di erent depths. From the measurement of the major ion concentrations, it was observed that the high-electric conductivity layers had di erent chemical characteristics. High concentrations of NO3 and SO42 deposits were observed in the snowpack layer that was formed due to the low-pressure system that passed in the vicinity of Japan. On the other hand, the layer that formed during the winter monsoon pattern, large amounts of sea salts were deposited in the snowpack in January 2007. However, layers with a high sea-salt concentration were not observed in February 2006. We analyzed the movement of the air mass that flowed into the study area. Air mass passed through the city at the time of the passage of the low-pressure system. In addition, the air mass that crossed the Sea of Japan entered the study area during the winter monsoon pattern. However, the movement of the air mass was di erent during the winter monsoon pattern in February 2006 and January 2007.
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
権利
権利情報 © 2008 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
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