Sea ice strength development from freezing to melting in the Antarctic marginal ice zone

F. Paul, T. Mielke, R. Audh, D. Lupascu
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Abstract

Sea ice growth in the Marginal Ice Zone of the Antarctic is one of the largest annual changes on earth with a huge impact on the global climate and ecology system. The principles of sea ice growth and melting in the MIZ of the Antarctic is yet not as well researched as its polar counterpart in the north.For this study, pancake ice, consolidated ice and floe ice were analyzed with a compression test in July, October and November 2019 in the marginal ice zone of the Antarctic. Newly formed pancake ice in July showed the highest compressive strength in the bottom layer (3 MPa), whereas consolidated ice was strongest at the top (5 MPa). Consolidated ice in October and November had the highest compressive strength in a middle layer with up to 13.5 MPa, the maximum strength at the top was 3 MPa. Floe ice, consisting of destroyed pack ice, did not show a clear strength development over sea ice depth.
南极边缘冰带海冰强度从冻结到融化的发展
南极边缘冰带的海冰增长是地球上最大的年度变化之一,对全球气候和生态系统产生巨大影响。南极MIZ地区海冰生长和融化的原理还没有像北极地区那样得到充分的研究。本研究于2019年7月、10月和11月对南极边缘冰带的煎饼冰、固结冰和浮冰进行了压缩试验分析。7月新形成的煎饼冰底部抗压强度最高(3 MPa),顶部固结冰最强(5 MPa)。10月和11月固结冰中层抗压强度最高,达13.5 MPa,顶层最大为3 MPa。由被破坏的浮冰组成的浮冰在海冰深度上没有显示出明显的强度发展。
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