首页> 外文会议>International conference on port and ocean engineering under arctic conditions >MEASUREMENTS OF ANTARCTIC SEA ICE THICKNESS DURING THE ICE TRANSIT OF S.A. AGULHAS Ⅱ
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MEASUREMENTS OF ANTARCTIC SEA ICE THICKNESS DURING THE ICE TRANSIT OF S.A. AGULHAS Ⅱ

机译:S.A.Agulhas冰川冰川Ⅱ期间南极海冰厚度的测量

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The South African polar supply icebreaker S.A. Agulhas Ⅱ was permanently instrumented for ice load measurements when built in Finland in 2012. The ship is used as a research platform during her annual relief voyages to Antarctica. The performance data is complemented with ice observations and ice thickness measurements using both electromagnetic (EM) method and stereocamera system. The thickness measurements are described and results from the first full campaign 2013-2014 are presented. The first period of ice transit extends from early December to early January while the latter covers late January and early February. Both include meridional transits between the ice margin and ice shelf, and zonal transits along the shelf. Six hour ice thickness averages grow gradually from 0.5 m of ice margin to 1 m at about 200 km from the shelf. This is followed by a transition to extremely deformed and 1.5-2 m thick near shelf ice types. The two types have different thickness distribution characteristics which is also reflected by the very large amount of ramming during the zonal transits. The EM results are in a good agreement with observations which also demonstrates that reliable thickness data can be obtained by careful observational methods. The reliability of shipborne thickness data to represent regional thickness variation is discussed and different ways to define the thickness distribution are compared.
机译:南非极性供应破冰船S.A.AgulhasⅡ在2012年在芬兰建造时永久借鉴冰负荷测量。该船在年度救济航行到南极洲的救济航行期间。使用电磁(EM)方法和立体声系统的冰观察和冰厚度测量,性能数据互补。描述了厚度测量并提出了第一全球活动2013-2014的结果。冰川的第一阶段从12月初到1月初,后者占1月底和2月初。两者都包括冰边缘和冰架之间的经透透支,以及沿着架子的区间途径。六小时冰厚度平均从0.5米的冰边坡逐渐增长至1米,距离架子约200公里。接下来这是一个过渡到极其变形和1.5-2米厚的架子冰类型。这两种类型具有不同的厚度分布特性,其也反映在区间期间的大量夯实。 EM结果与观察结果良好,也表明通过仔细观察方法可以获得可靠的厚度数据。讨论了船载厚度数据的可靠性,以表示区域厚度变化,并进行了不同的方式来定义厚度分布。

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