Antarctic Bottom Water production from the Vincennes Bay Polynya, East Antarctica

被引:46
作者
Kitade, Yujiro [1 ]
Shimada, Keishi [1 ]
Tamura, Takeshi [2 ,3 ]
Williams, Guy D. [3 ]
Aoki, Shigeru [4 ]
Fukamachi, Yasushi [4 ]
Roquet, Fabien [5 ]
Hindell, Mark [6 ]
Ushio, Shuki [2 ]
Ohshima, Kay I. [4 ]
机构
[1] Tokyo Univ Marine Sci & Technol, Tokyo, Japan
[2] Natl Inst Polar Res, Tachikawa, Tokyo, Japan
[3] Univ Tasmania, Antarctic Climate & Ecosyst Cooperat Res Ctr, Hobart, Tas, Australia
[4] Hokkaido Univ, Inst Low Temp Sci, Sapporo, Hokkaido 060, Japan
[5] Stockholm Univ, Dept Meteorol, S-10691 Stockholm, Sweden
[6] Univ Tasmania, Inst Marine & Antarctic Studies, Hobart, Tas, Australia
关键词
Antarctic Bottom Water; dense shelf water; sea-ice production; Australian-Antarctic Basin; polynya; 140-DEGREES-E; CIRCULATION; ZONE;
D O I
10.1002/2014GL059971
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
One year moorings at depths greater than 3000m on the continental slope off Vincennes Bay, East Antarctica, reveal the cold (<-0.5 degrees C) and fresh (<34.64) signals of newly formed Antarctic Bottom Water (AABW). The signal appeared in June, 3 months after the onset of active sea-ice production in the nearby Vincennes Bay Polynya (VBP). The AABW signal continued for about 5 months at two moorings, with 1 month delay at the western site further downstream. Ship-based hydrographic data are in agreement, detecting the westward spread of new AABW over the continental slope from VBP. On the continental shelf, Dense Shelf Water (DSW) formation is observed by instrumented seals, in and around the VBP during autumn, and we estimate its transport to be 0.16 +/- 0.07 (x 106m3s-1). We conclude that the DSW formed in this region, albeit from a modest amount of sea-ice production, nonetheless contributes to the upper layer of AABW in Australian-Antarctic Basin.
引用
收藏
页码:3528 / 3534
页数:7
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