Massive subsurface ice formed by refreezing of ice-shelf melt ponds

被引:65
|
作者
Hubbard, Bryn [1 ]
Luckman, Adrian [2 ]
Ashmore, David W. [1 ]
Bevan, Suzanne [2 ]
Kulessa, Bernd [2 ]
Munneke, Peter Kuipers [2 ]
Philippe, Morgane [3 ]
Jansen, Daniela [4 ]
Booth, Adam [5 ]
Sevestre, Heidi [6 ]
Tison, Jean-Louis [3 ]
O'Leary, Martin [2 ]
Rutt, Ian [2 ]
机构
[1] Aberystwyth Univ, Dept Geog & Earth Sci, Ctr Glaciol, Aberystwyth SY23 3DB, Dyfed, Wales
[2] Swansea Univ, Dept Geog, Glaciol Grp, Swansea SA2 8PP, W Glam, Wales
[3] Univ Libre Bruxelles, Lab Glaciol, Dept Geosci Environm & Soc, B-1050 Brussels, Belgium
[4] Helmholtz Zentrum Polar & Meeresforsch, Alfred Wegener Inst, D-27568 Bremerhaven, Germany
[5] Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England
[6] Univ Ctr Svalbard, Dept Arctic Geol, N-9171 Longyearbyen, Norway
来源
NATURE COMMUNICATIONS | 2016年 / 7卷
基金
英国自然环境研究理事会;
关键词
ANTARCTIC PENINSULA; SURFACE; BOREHOLE; STABILITY; GLACIER; CLIMATE; BALANCE; WATER;
D O I
10.1038/ncomms11897
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Surface melt ponds form intermittently on several Antarctic ice shelves. Although implicated in ice-shelf break up, the consequences of such ponding for ice formation and ice-shelf structure have not been evaluated. Here we report the discovery of a massive subsurface ice layer, at least 16 km across, several kilometres long and tens of metres deep, located in an area of intense melting and intermittent ponding on Larsen C Ice Shelf, Antarctica. We combine borehole optical televiewer logging and radar measurements with remote sensing and firn modelling to investigate the layer, found to be similar to 10 degrees C warmer and B170 kgm(-3) denser than anticipated in the absence of ponding and hitherto used in models of ice-shelf fracture and flow. Surface ponding and ice layers such as the one we report are likely to form on a wider range of Antarctic ice shelves in response to climatic warming in forthcoming decades.
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页数:6
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