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Effects of intraseasonal variations of the Arctic Oscillation on the Barents Sea
https://doi.org/10.15094/00002974
https://doi.org/10.15094/00002974e5d1d5ba-a465-40b7-ace6-a032ede4b9bd
名前 / ファイル | ライセンス | アクション |
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KJ00001036820 (5.3 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 2004-11-01 | |||||
タイトル | ||||||
タイトル | Effects of intraseasonal variations of the Arctic Oscillation on the Barents Sea | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Arctic Oscillation, North Atlantic water, Barents Sea, sea ice, sea water temperature | |||||
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 | 10.15094/00002974 | |||||
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) | |||||
論文名よみ | ||||||
その他のタイトル | Effects of intraseasonal variations of the Arctic Oscillation on the Barents Sea | |||||
著者名(英) |
Wu,Bingyi
× Wu,Bingyi× Wang,Jia× Zhang,Renhe |
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著者所属(英) | ||||||
en | ||||||
Chinese Academy of Meteorological Sciences/International Arctic Research Center, University of Alaska Fairbanks/Chinese Academy of Meteorological Sciences | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | This paper investigates possible connections among the wintertime Arctic Oscillation(AO), North Atlantic water inflow into the Barents Sea, and sea ice and sea water temperature in the Barents Sea on monthly to seasonal time scales using a coupled sea-ice-ocean model. The forcing is from winters with large anomalies of the AO. The inflow of the North Atlantic water into the Barents Sea forced by significantly different wind stresses over the area south of the Barents Sea shows a close relation to the AO only during the AO high-phase periods rather than during the low-phase periods. The responses to forcing by the opposite phases of the AO differ substantially in surface and subsurface water temperature of the Barents Sea. The positive phase of the AO raises subsurface water temperature in the Barents Sea, with concurrent surface cooling in the western and central Barents Sea. One exception is in the eastern Barents Sea where the surface water temperature is higher during the positive phase than during the negative phase. The enhanced net inflow of warmer Atlantic water into the Barents Sea causes decrease of sea ice. | |||||
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 18, p. 82-95, 発行日 2004-11 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |