Past and future grounding-line retreat of the West Antarctic Ice Sheet

被引:333
作者
Conway, H [1 ]
Hall, BL
Denton, GH
Gades, AM
Waddington, ED
机构
[1] Univ Washington, Geophys Program, Seattle, WA 98195 USA
[2] Univ Maine, Inst Quaternary Studies, Orono, ME 04469 USA
[3] Univ Maine, Dept Geol Sci, Orono, ME 04469 USA
[4] Woods Hole Oceanog Inst, Dept Geol & Geophys, Woods Hole, MA 02543 USA
关键词
D O I
10.1126/science.286.5438.280
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
The history of deglaciation of the West Antarctic Ice Sheet (WAIS) gives clues about its future. Southward grounding-line migration was dated past three Locations in the Ross Sea Embayment. Results indicate that most recession occurred during the middle to Late Holocene in the absence of substantial sea Level or climate forcing. Current grounding-line retreat may reflect ongoing ice recession that has been under way since the early Holocene. If so, the WAIS could continue to retreat even in the absence of further external forcing.
引用
收藏
页码:280 / 283
页数:4
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