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- Aoki S.
- Institute of Low Temperature Science, Hokkaido University
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- Bajish C. C.
- Graduate School of Environmental Science, Hokkaido University
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- Taguchi B.
- Earth Simulator Center, JAMSTEC
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- Komori N.
- Earth Simulator Center, JAMSTEC
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- Kim S.-J.
- Korea Polar Research Institute, KIOST
書誌事項
- 公開日
- 2013
- 資源種別
- journal article
- DOI
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- 10.2151/sola.2013-008
- 公開者
- 公益社団法人 日本気象学会
説明
Decadal variability of Antarctic sea ice and a role of ocean dynamics are examined with sea ice concentration (SIC) and sea surface temperature (SST) derived from satellite microwave observation and obtained by a high resolution coupled ocean-atmosphere-ice general circulation model (CGCM). Sea ice observations revealed a circumpolar variability of sea ice edge (SIE) on quasi-decadal time scale. SST also showed variation on similar time scale with warm (cool) anomaly roughly corresponding to retreat (extension) of SIE at negative (positive) southern annular mode (SAM). CGCM run without anthropogenic forcing and volcanic eruptions revealed that the leading mode of SIC is quasi-circumpolar pattern with a dominant time scale of 12-17 years and the leading mode of SST also has a similar pattern with the SIC showing a high degree of inverse correlation. The modeled SAM significantly correlates with these leading modes of both SIC and SST, representing the same structure with the observations. This indicates that the oceanic natural variability is the key to understand the quasi-decadal variability in sea ice.
収録刊行物
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- SOLA
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SOLA 9 (0), 32-35, 2013
公益社団法人 日本気象学会
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詳細情報 詳細情報について
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- CRID
- 1390001205221224192
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- NII論文ID
- 130004448594
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- ISSN
- 13496476
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- 本文言語コード
- en
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- 資料種別
- journal article
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- データソース種別
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- JaLC
- Crossref
- CiNii Articles
- KAKEN
- OpenAIRE
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- 抄録ライセンスフラグ
- 使用不可
