Marine ice regulates the future stability of a large Antarctic ice shelf.

Marine ice regulates the future stability of a large Antarctic ice shelf.
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DOI:
10.1038/ncomms4707
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发表时间:
2014-04-22
影响因子:
16.6
通讯作者:
Sammonds, Peter R.
Sammonds, Peter R.
中科院分区:
综合性期刊1区
文献类型:
--
作者:
Kulessa, Bernd;Jansen, Daniela;Luckman, Adrian J.;King, Edward C.;Sammonds, Peter R.

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1995年和2002年南极半岛拉森A和B冰架的崩塌证实了气候变暖向南传播对该地区的影响。Larsen B的南部邻居Larsen C是南极洲第四大冰架,最近的质量和动力变化可能预示着类似的不稳定性。在这里,使用经过验证的冰架模型运行在诊断模式下,卫星和现场地球物理数据的约束,我们确定这种潜在的不稳定性的性质。我们证明,目前的空间分布和方向的主应力在拉森C冰架内类似于那些在崩溃前拉森B。当拉森B的稳定锋面部分在1995年消失时,剩下的不稳定的大陆架加速,崩溃并最终崩溃。我们假设,拉森C冰架可能会遭受类似的命运,如果它不稳定的温暖和机械柔软的海冰,夹带在狭窄的缝合带。 南极拉森C冰架的不稳定迹象引发了人们的担忧,即它可能很快就会像它的北方邻居拉森B一样崩溃。Kulessa等人将联合收割机的冰架模型与卫星和地球物理数据相结合,表明尽管动力学相似,但Larsen C目前是由海冰稳定的。
The collapses of the Larsen A and B ice shelves on the Antarctic Peninsula in 1995 and 2002 confirm the impact of southward-propagating climate warming in this region. Recent mass and dynamic changes of Larsen B’s southern neighbour Larsen C, the fourth largest ice shelf in Antarctica, may herald a similar instability. Here, using a validated ice-shelf model run in diagnostic mode, constrained by satellite and in situ geophysical data, we identify the nature of this potential instability. We demonstrate that the present-day spatial distribution and orientation of the principal stresses within Larsen C ice shelf are akin to those within pre-collapse Larsen B. When Larsen B’s stabilizing frontal portion was lost in 1995, the unstable remaining shelf accelerated, crumbled and ultimately collapsed. We hypothesize that Larsen C ice shelf may suffer a similar fate if it were not stabilized by warm and mechanically soft marine ice, entrained within narrow suture zones. Signs of instability in the Antarctic Larsen C ice shelf have raised concerns that it might soon collapse like its northern neighbour Larsen B. Kulessa et al. combine an ice-shelf model with satellite and geophysical data to show that despite dynamic similarities, Larsen C is presently stabilized by marine ice.
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