Under Ice-Shelf Eddy at the Stancomb-Wills Ice Tongue

IF 3.3 2区 地球科学 Q1 OCEANOGRAPHY
C. Hancock, K. Speer, M. Janout, O. Boebel
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Abstract

Eddies are considered important for the dynamics within the Antarctic Slope Current but are difficult to observe due to the often year-round ice cover in the southern Weddell Sea. Here we present novel findings from acoustically tracked profiling floats, which observed the spin-down of an eddy under an ice shelf. Two profiling floats were deployed at 8°W in the Antarctic Slope Current and drifted westward along the slope at 800 m depth. One of the floats was captured by an anticyclonic eddy in the wake of the Riiser-Larsen Ice shelf. We postulate the eddy was generated by baroclinic instability due to the interaction of the Antarctic Slope Current with floating ice shelves. Float trajectories show the eddy propagated westward along the slope and ultimately became trapped under the Stancomb-Wills Ice Tongue, where the eddy spun down because of ocean-ice shelf stresses. Simple bulk mixing calculations were fitted to observations to explore the role of eddies under the ice shelf, in relation to an “Eddy-Ice-Pumping” mechanism, and revealed that significant basal melting occurred. Subsequent vertical mixing of the eddy's cold and fresh core, due to the Eddy-Ice-Pumping mechanism, resulted in a cold and fresh subsurface signal which was still evident downstream at the Filchner Trough 3 months later. Estimates of eddy contributions to basal melt and freshwater transport show eddies could have a significant impact on the stratification and thermocline depth downstream, potentially affecting the inflow of modified Warm Deep Water into the Filchner Trough.

Abstract Image

斯坦库姆-威尔斯冰舌的冰架旋涡下
涡旋被认为对南极坡流内部的动力学很重要,但由于威德尔海南部经常全年被冰覆盖,因此很难观测到。在这里,我们提出了声学跟踪剖面浮标的新发现,该浮标观察到冰架下涡流的自旋下降。两个剖面浮标部署在南极坡流8°W处,沿坡向西漂移800 m深度。其中一个漂浮物被里瑟-拉森冰架后的反气旋涡流捕获。我们假定涡旋是由南极坡流与浮冰架相互作用引起的斜压不稳定所产生的。浮子轨迹显示涡旋沿着斜坡向西传播,最终被困在斯坦库姆-威尔斯冰舌下,在那里涡旋由于海洋冰架的压力而旋转下来。简单的体积混合计算与观测相吻合,以探索冰架下漩涡的作用,与“漩涡-冰泵”机制有关,并揭示了显著的基底融化发生。由于涡旋-抽冰机制,随后涡旋的冷芯和新鲜芯的垂直混合导致了3个月后在Filchner海槽下游仍然明显的冷芯和新鲜地下信号。涡旋对基底融化和淡水运输的贡献估计表明,涡旋可能对下游的分层和温跃层深度产生重大影响,可能影响经过改造的暖深水流入Filchner海槽。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Journal of Geophysical Research-Oceans
Journal of Geophysical Research-Oceans Earth and Planetary Sciences-Oceanography
CiteScore
7.00
自引率
13.90%
发文量
429
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