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北出, 裕二郎
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第54次日本南極地域観測隊東京海洋大学研究練習船「海鷹丸」(KARE16...
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第54次日本南極地域観測隊東京海洋大学研究練習船「海鷹丸」(KARE16...
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Effects of cabbeling and thermobaricity on AABW and MCDW formation around 110°E-...
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Characteristics of bottom boundary mixing across the shelf edge off Cape Darnley...
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第52次日本南極地域観測隊夏隊における東京海洋大学「海鷹丸」観測報告...
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Absolute velocity field of Antarctic Slope Current and topographically constrain...
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The possibility of Antarctic Bottom Water originating from middle size Polynya a...
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南極底層水を起点とする熱塩循環・物質循環のダイナミクス...
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Properties of Antarctic Bottom Water observed by mooring system off Vincennes Ba...
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Rapid and persistent freshening of Antarctic Bottom Water in the Australian-Anta...
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カイヨウ シンソウ ダイジュンカン ニ ゲキヘン ノ キザシ オ ケンシュツ ~ テイミツドカ ニ ヨリ ナンキョク タイリク エンペン ノ シズメヌ レイスイ...
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南大洋の上層における季節変動と力学
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551.46
南大洋
南極底層水
南極底層水の昇温・低塩化に伴う深層大循環の変貌予測に関する基礎研究
南極海
海洋物理化学基本観測
生態系変動
Basic research on the prediction of changing for the Deep Global Circulation related with warming and freshening of Antarctic Bottom Water
Elucidation of the formation mechanisms of the large standing oceanic eddy and the factors controlling eddy circulation contributing to warm water transport to the Totten Ice Shelf in East Antarctica
東南極トッテン棚氷へ暖水を運ぶ巨大な定在海洋渦の成因と循環流量の変動要因の解明
科学研究費研究成果
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