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Polar ice sheets: a review

Published online by Cambridge University Press:  27 October 2009

G. de Q. Robin
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At the present time, only Antarctica and Greenland carry ice sheets comparable with the ice sheets that covered vast areas of the Northern Hemisphere as recently as 20 000 years ago. At the time of maximum glaciation, some 300 000 years ago, the volume of ice on earth was three times what it is today, and it covered the northern parts of continents all around the Arctic Ocean. In North America, ice stretched south as far as Kansas; in Europe, it extended down ot the River Thames and the Sudety mountains and covered much of Siberia. Even now, the Antarctic ice sheet covers an area of 12 million km2 and in places reaches depths of more than 4 km. The smaller Greenland ice sheet has an area of 1.8 million km2 and exceeds 3 km in depth.

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Articles
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Polar Record , Volume 16 , Issue 100 , January 1972, pp. 5 - 22
Copyright
Copyright © Cambridge University Press 1972

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References

Budd, W. F., Jenssen, D. and Radok, U. 1971. Derived physical characteristics of the Antarctic ice sheet, Mark I. University of Melbourne Meteorology Departmentv Publication No 18.Google Scholar
Budd, W. F. and Radok, U. 1971. Glaciers and other large ice masses. Reports on Progress in Physics, Vol 34, No 1, p 1–70.Google Scholar
Dansgaard, W., Johnsen, S. J., Møller, J. and Langway, C. C. Jr 1970. Oxygen isotope analysis of a core representing a complete vertical profile of a polar ice sheet In: Gow, A. J.and others, eds. International Symposium on Antarctic Glaciological Exploration (ISAGE). . . 1968 . . . Gentbrugge, International Association of Scientific Hydrology [etc], p 93–94 (Publication No 86 of the IASH).Google Scholar
Drewry, D. J. (in press). [Subglacial morphology between the Transantarctic Mountains and the South Pole.] In: Adie, R. J.ed. Symposium on Antarctic Geology and Solid Earth Geophysics, 1970.Google Scholar
Epstein, S., Sharp, R. P. and Gow, A. G. 1970. Antarctic ice sheet: stable isotope analyses of Bryd station cores and interhemispheric climatic implications. Science, Vol 168, No 3939, p 1570–72.CrossRefGoogle Scholar
Giovinetto, M. B., Robinson, E. S. and Swtthinbank, C. W. M. 1966. The regime of the western part of the Ross Ice Shelf drainage system. Journal of Glaciology, Vol 6, No 43, p 55–68.CrossRefGoogle Scholar
Langway, C. C. Jr and Hansen, , Lyle, B.. 1970. Drilling through the ice cap. Bulletin of the Atomic Scientists, Vol 26, No 10, p 63–66.CrossRefGoogle Scholar
Robin, G. de Q. 1955. Ice movement and temperature distribution in glaciers and ice sheets. Journal of Glaciology, Vol 2, No 18, p 523–32.CrossRefGoogle Scholar
Robin, G. de Q., Swtthinbank, C. W. M. and Smith, B. M. E. 1970. Radio echo exploration of the Antarctic ice sheet In: Gow, A. J.and others, eds. International Symposium on Antarctic Glaciological Exploration (ISAGE) . . . 1968 . . . Gentbrugge, International Association of Scientific Hydrology [etc], p 97–114.Google Scholar
Thomas, R. H. and Coslett, P. H. 1970. Bottom melting of ice shelves and the mass balance of Antarctica. Nature, Vol 228, No 5266, p 47–49.CrossRefGoogle ScholarPubMed