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Far-Reaching Effects of Okhotsk Sea Ice Area on Sea Surface Heat Flux, Lower Atmosphere, and Ocean Mixed Layer
https://fra.repo.nii.ac.jp/records/2001426
https://fra.repo.nii.ac.jp/records/2001426227deebc-d76d-42e1-a248-07b24c9ac98f
名前 / ファイル | ライセンス | アクション |
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Item type | 学術雑誌論文 / Journal Article(1) | |||||||||||||||||||||||||||||
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公開日 | 2024-03-14 | |||||||||||||||||||||||||||||
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言語 | en | |||||||||||||||||||||||||||||
タイトル | Far-Reaching Effects of Okhotsk Sea Ice Area on Sea Surface Heat Flux, Lower Atmosphere, and Ocean Mixed Layer | |||||||||||||||||||||||||||||
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言語 | eng | |||||||||||||||||||||||||||||
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言語 | en | |||||||||||||||||||||||||||||
主題Scheme | Other | |||||||||||||||||||||||||||||
主題 | Sea ice; Atmosphere–ocean interaction; Oceanic mixed layer; Heat budgets/fluxes; Surface temperature; Interannual variability | |||||||||||||||||||||||||||||
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資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||||||||||||||||||||||||
資源タイプ | journal article | |||||||||||||||||||||||||||||
著者 |
中村, 知裕
× 中村, 知裕
× 高橋, 祐輔
× 中野渡, 拓也
WEKO
1013
× 三寺, 史夫
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内容記述タイプ | Abstract | |||||||||||||||||||||||||||||
内容記述 | The impact of interannual variations in sea ice area in the Okhotsk Sea was investigated through a composite analysis of years with extensive and limited sea ice areas (referred to as heavy and light ice years, respectively), using atmospheric and oceanic reanalysis data. The comparison of heavy and light ice-year composites in February revealed a substantial decrease in upward surface turbulent heat flux in the Okhotsk Sea (∼−250 W m−2) and a notable increase in a surprisingly extensive region in the western North Pacific (30–120 W m−2), spanning 2300 km from the ice edge. These differences were consistent with the decrease in surface air temperature and specific humidity, suggesting that during heavy ice years, cold and dry air blowing from Siberia to the North Pacific via the Okhotsk Sea undergoes less modification over larger sea ice areas, remaining colder and drier in the North Pacific and thereby enhancing the heat flux. Such advection can be associated with the Asian winter monsoon and migratory cyclones. Cloud cover and surface radiation flux altered consistently with these differences, although longwave and shortwave radiation largely counterbalanced each other. Additionally, the Pacific storm track exhibited variation. In accordance with the heat flux difference, sea surface temperature decreased, and the ocean mixed layer deepened around the subarctic during heavy ice years. These findings suggest that sea ice area in the Okhotsk Sea influences the lower atmosphere and surface ocean in the North Pacific. Such impacts could further affect ocean nutrient circulation, ecosystems, and atmospheric teleconnections. | |||||||||||||||||||||||||||||
言語 | en | |||||||||||||||||||||||||||||
書誌情報 |
en : Journal of Climate 巻 37, 号 2, p. 569-583, ページ数 15, 発行日 2024-01-15 |
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言語 | en | |||||||||||||||||||||||||||||
出版者 | American Meteorological Society | |||||||||||||||||||||||||||||
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収録物識別子タイプ | PISSN | |||||||||||||||||||||||||||||
収録物識別子 | 0894-8755 | |||||||||||||||||||||||||||||
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識別子タイプ | DOI | |||||||||||||||||||||||||||||
関連識別子 | 10.1175/JCLI-D-23-0239.1 | |||||||||||||||||||||||||||||
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関連タイプ | isIdenticalTo | |||||||||||||||||||||||||||||
識別子タイプ | Local | |||||||||||||||||||||||||||||
関連識別子 | 23235012 | |||||||||||||||||||||||||||||
言語 | ja | |||||||||||||||||||||||||||||
関連名称 | 水産資源研究所 水産資源研究センター 海洋環境部 | |||||||||||||||||||||||||||||
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識別子タイプ | URI | |||||||||||||||||||||||||||||
関連識別子 | https://journals.ametsoc.org/view/journals/clim/37/2/JCLI-D-23-0239.1.xml | |||||||||||||||||||||||||||||
言語 | en | |||||||||||||||||||||||||||||
関連名称 | AMS | |||||||||||||||||||||||||||||
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出版タイプ | VoR | |||||||||||||||||||||||||||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |