Subglacial floods beneath ice sheets

被引:84
作者
Evatt, G. W.
Fowler, A. C.
Clark, C. D.
Hulton, N. R. J.
机构
[1] Univ Oxford, Inst Math, Oxford OX1 3LB, England
[2] Univ Sheffield, Dept Geog, Sheffield S10 2TN, S Yorkshire, England
[3] Univ Edinburgh, Sch Geosci, Edinburgh EH8 9XP, Midlothian, Scotland
来源
PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES | 2006年 / 364卷 / 1844期
关键词
jokulhlaups; ice sheets; subglacial hydrology; Dansgaard-Oeschger events; sub-Antarctic lakes;
D O I
10.1098/rsta.2006.1798
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
Subglacial floods (jokulhlaups) are well documented as occurring beneath present day glaciers and ice caps. In addition, it is known that massive floods have occurred from ice-dammed lakes proximal to the Laurentide ice sheet during the last ice age, and it has been suggested that at least one such flood below the waning ice sheet was responsible for a dramatic cooling event some 8000 years ago. We propose that drainage of lakes from beneath ice sheets will generally occur in a time-periodic fashion, and that such floods can be of severe magnitude. Such hydraulic eruptions are likely to have caused severe climatic disturbances in the past, and may well do so in the future.
引用
收藏
页码:1769 / 1794
页数:26
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