| Item type |
学術雑誌論文 / Journal Article(1) |
| 公開日 |
2007-06-13 |
| タイトル |
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|
タイトル |
Regional characteristics of chemical constituents in surface snow, Arctic cryosphere |
|
言語 |
en |
| 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 |
| アクセス権 |
|
|
アクセス権 |
open access |
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アクセス権URI |
http://purl.org/coar/access_right/c_abf2 |
| 著者 |
Motoyama, Hideaki
Watanabe, Okitsugu
Kamiyama, Kokichi
Igarashi, Makoto
Goto-Azuma, Kumiko
Fujii, Yoshiyuki
Iizuka, Yoshinori
Matoba, Sumito
Narita, Hideki
Kameda, Takao
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| 著者別名 |
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識別子Scheme |
WEKO |
|
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識別子 |
44128 |
|
|
識別子Scheme |
KAKEN |
|
|
識別子URI |
https://nrid.nii.ac.jp/ja/nrid/1000000233974 |
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|
識別子 |
233974 |
|
|
姓名 |
亀田, 貴雄 |
|
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言語 |
ja |
| 抄録 |
|
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内容記述タイプ |
Abstract |
|
内容記述 |
Surface snow observations were carried out on many glaciers in the Arctic. The observational sites were in Svalbard，Severnaya Zemlya，Greenland and arctic Canada. The seasonal variations of chemical constituents in snowfall remained in the surface snow on the central Greenland ice sheet where the effect of snowmelt was weak. Conversely, the chemical constituents in the snow layer changed with infiltration of melt water on the Svalbard glacier where strong snowmelt occurred，even in high latitudes. But in general, specific regional characteristics remained in all the glaciers. The concentrations of ions in snow were significantly decreased，because of percolation of melt water. But the ratio of NO_3 to CI still had unique regional characteristic values． |
| 書誌情報 |
Polar Meteorology and Glaciology
巻 15,
p. 55-66,
発行日 2001-11
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| 権利 |
|
|
権利情報 |
NATIONAL INSTITUTE OF POLAR RESEARCH, H.Motoyama, O.Watanabe, K.Kamiyama, M.Igarashi, K.Koto-Azuma, Y.Fujii, Y.Iizuka, S.Matoba, H.Narita, T.Kameda, Polar Meteorology and Glaciology, 15, 2001, 55-66. |
| フォーマット |
|
|
内容記述タイプ |
Other |
|
内容記述 |
application/pdf |
| 出版者 |
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|
出版者 |
国立極地研究所 |
|
言語 |
ja |
| 著者版フラグ |
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|
言語 |
en |
|
値 |
publisher |
| 出版タイプ |
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|
出版タイプ |
VoR |
|
出版タイプResource |
http://purl.org/coar/version/c_970fb48d4fbd8a85 |
4491.pdf (4.8 MB)
