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Characteristics of summer water balance in eastern Siberian tundra watershed
https://doi.org/10.15094/00002933
https://doi.org/10.15094/0000293328dc1189-21ab-4d05-bca6-08af154b4df7
名前 / ファイル | ライセンス | アクション |
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KJ00002364420 (1.7 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 2001-11-01 | |||||
タイトル | ||||||
タイトル | Characteristics of summer water balance in eastern Siberian tundra watershed | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15094/00002933 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
記事種別(英) | ||||||
en | ||||||
Scientific Paper | ||||||
論文名よみ | ||||||
その他のタイトル | Characteristics of summer water balance in eastern Siberian tundra watershed | |||||
著者名よみ |
サトウ, ノリフミ
× サトウ, ノリフミ× イシイ, ヨシユキ× コダマ, ユウジ× ノムラ, ムツミ× イシカワ, ノブヨシ× コバヤシ, ダイジ |
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著者名(英) |
Sato, Norifumi
× Sato, Norifumi× Ishii, Yoshiyuki× Kodama, Yuji× Nomura, Mutsumi× Ishikawa, Nobuyoshi× Kobayashi, Daiji |
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著者所属(英) | ||||||
en | ||||||
Institute of Low Temperature Science, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
Institute of Low Temperature Science, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
Institute of Low Temperature Science, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
University Forest, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
Institute of Low Temperature Science, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
Institute of Low Temperature Science, Hokkaido University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Hydrological observations were carried out in a tundra watershed near Tiksi, eastern Siberia during summer in 1997,1998 and 1999,and characteristics of the summer water balance are discussed. Due to strong wind in winter and low height vegetation, snowdrift is a common feature in the tundra area, and remain as snow patches until the middle of summer, supplying meltwater to rivers. In the summer water balance analysis, we introduced the ratio α of the snow patch area to the whole watershed area as a tuning parameter for taking into account the meltwater from the snow patches. The obtained results are as follows : The contribution of meltwater from snow patches to discharge continued in summer after the main snowmelt period. Rainfall and snowmelt amount changed substantially from year to year. The major output component was discharge. The contribution of evapotranspiration to the output varied year to year. The storage change was small compared with the other components. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1129795X | |||||
書誌情報 |
Polar meteorology and glaciology 巻 15, p. 91-106, 発行日 2001-11 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |