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Global Climate Change DigestArchives of the
Global Climate Change Digest

A Guide to Information on Greenhouse Gases and Ozone Depletion
Published July 1988 through June 1999

FROM VOLUME 4, NUMBER 12, DECEMBER 1991

PROFESSIONAL PUBLICATIONS...
ANTARCTIC ICE SHEET


Item #d91dec46

"Changes in the West Antarctic Ice Sheet," R.B. Alley (Earth Syst. Sci. Ctr., 306 Deike Bldg., Pennsylvania State Univ., Univ. Pk. PA 16802), I.M. Whillans, Science, 254(5034), 959-963, Nov. 15, 1991.

The portion of the ice sheet that flows into the Ross Sea is thinning in some places and thickening in others, because of a delayed response to the end of the last global glacial cycle as well as internal instability, not because of any current climate change. Its near-future impact on global sea level is thus already determined regardless of climate change, but too little of the ice sheet has been surveyed to predict its overall future behavior.


Item #d91dec47

"Evidence from Antarctic Ice Cores for Recent Increases in Snow Accumulation," V.I. Morgan (Australian Antarctic Div., Channel Hwy., Kingston 7050, Australia), I.D. Goodwin et al., Nature, 354(6348), 58-60, Nov. 7, 1991.

A time series of the net rate of snow accumulation since 1806, derived from the thicknesses of annual layers in ice cores, shows an increase to about 20% above the long-term mean following a minimum around 1960. Other data suggest this increase is widespread over Antarctica and should contribute to a lowering of sea level of 1.0-1.2 mm per year.


Item #d91dec48

"Advance of East Antarctic Outlet Glaciers During the Hypsothermal: Implications for the Volume State of the Antarctic Ice Sheet Under Global Warming," E.W. Domack (Dept. Geol., Hamilton College, Clinton NY 13323), A.J.T. Jull, S. Nakao, Geology, 19, 1059-1062, Nov. 1991.

Radiocarbon dating of sediments, from three sites near ice shelves or smaller ice tongues close to outlet glaciers, established the history of ice advances or retreats reflected respectively in alternating layers of glacial debris or remains of marine algae. Antarctic ice fringes have advanced during past warm intervals, and reached their greatest extent 4,000-7,000 years ago, when global temperatures were 1° or 2° C warmer than present.


Item #d91dec49

"Quaternary and Tertiary Microfossils from Beneath Ice Stream B: Evidence for a Dynamic West Antarctic Ice Sheet History," R.P. Scherer (Polar Res. Ctr., Ohio State Univ., Columbus OH 43210), Palaeogeog., Palaeoclim., Palaeoecol., (Global Planet. Change Sec.), 90(4), 395-412, Oct. 1991.

Some glaciologists have suggested that the ice sheet, which is grounded below sea level, could become unstable and disintegrate, but geologic evidence of such an occurrence in the past has been lacking. This study found evidence in sediments of ice-free conditions during certain Cenozoic intervals, lending credence to the concern that global warming and rising sea levels could lead to collapse of the ice sheet in the near future.

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