A NOTE ON WATER EXCHANGE UNDER FAST ICE IN LUTZOW-HOLM BAY, ANTARCTICA
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概要
- 論文の詳細を見る
Under coastal fast ice in the Ongul Strait near Syowa Station, Antarctica, warmer, more saline, and oxygen-poorer water appears in mid-depth and deep layers from winter to spring every year. This water is explained as a result of mixing between Circumpolar Deep Water (CDW) and Winter Water (WW). This water becomes more like CDW and more homogenized with time from winter to spring, and in December a mixing ratio of 1 : 3-1 : 4 for CDW to WW is required to explain the properties of the homogenized water. It is inferred that the CDW comes along the glacial troughs. Transport of CDW results in a significant amount of heat supply into the water under fast ice.
- 国立極地研究所の論文
著者
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Ushio Shuki
Institute Of Low Temperature Science Hokkaido University
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ONO Nobuo
National Institute of Polar Research
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Takizawa Takatoshi
Japan Marine Science and Technology Center
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TAKIZAWA Takatoshi
Institute of Low Temperature Science, Hokkaido University
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OHSHIMA Kay
Institute of Low Temperature Science, Hokkaido University
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ONO Nobuo
Institute of Low Temperature Science, Hokkaido University
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Ohshima K
Hokkaido Univ. Sapporo Jpn
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Ohshima Kay
The Institute Of Low Temperature Science Hokkaido University
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Ohshima Kay
Hokkaido Univ. Sapporo Jpn
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Ohshima Kay
Institute Of Low Temperature Science Hokkaido University
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Ohshima Kay
Institute Of Llow Temperature Science Hokkaido University
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Ono N
National Institute Of Polar Research
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Ono Nobuo
Institute Of Low Temperature Science Hokkaido University
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