Basal channels drive active surface hydrology and transverse ice shelf fracture.
Basal channels drive active surface hydrology and transverse ice shelf fracture.
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DOI:
10.1126/sciadv.aao7212
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发表时间:
2018-06
期刊:
影响因子:
13.6
通讯作者:
Zappa CJ
中科院分区:
文献类型:
--
作者:
Dow CF;Lee WS;Greenbaum JS;Greene CA;Blankenship DD;Poinar K;Forrest AL;Young DA;Zappa CJ
Ice shelf basal channels cause transverse fractures that can be exacerbated by surface rivers, culminating in calving. Ice shelves control sea-level rise through frictional resistance, which slows the seaward flow of grounded glacial ice. Evidence from around Antarctica indicates that ice shelves are thinning and weakening, primarily driven by warm ocean water entering into the shelf cavities. We have identified a mechanism for ice shelf destabilization where basal channels underneath the shelves cause ice thinning that drives fracture perpendicular to flow. These channels also result in ice surface deformation, which diverts supraglacial rivers into the transverse fractures. We report direct evidence that a major 2016 calving event at Nansen Ice Shelf in the Ross Sea was the result of fracture driven by such channelized thinning and demonstrate that similar basal channel–driven transverse fractures occur elsewhere in Greenland and Antarctica. In the event of increased basal and surface melt resulting from rising ocean and air temperatures, ice shelves will become increasingly vulnerable to these tandem effects of basal channel destabilization.
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