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GEOPHYSICAL RESEARCH LETTERS,
VOL. 28, NO. 2,
PAGES 307–310,
2001
Future of the Arctic Sea Ice Cover: Implications of an Antarctic Analog
Douglas G. Martinson
Lamont-Doherty Earth Observatory, and Department of Earth and Environmental Sciences, Columbia University, Palisades, NY 10964
Michael Steele
Polar Science Center, Applied Physics Laboratory, University of Washington, Seattle, WA 98105
Abstract
Recent observations reveal a significant change in the upper ocean characteristics of the eastern Arctic in 1995. The change
is manifested through the loss of a near-surface layer known as the cold halocline layer (CHL). Without the CHL, the Arctic
water column looks and behaves like the Antarctic water column. The expected local impact is the appearance of significant
winter ocean heat fluxes (15 - 20 W/m²) and reduction of winter ice growth by 70 - 80% relative to years in which the CHL was present. Preliminary results suggest
a partial recovery of the CHL in the late 1990’s, tracking the weakening of the Arctic Oscillation.
Received 22
February
2000;
accepted 11
July
2000.
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Citation: Martinson, D. G., and M. Steele
(2001),
Future of the Arctic Sea Ice Cover: Implications of an Antarctic Analog,
Geophys. Res. Lett.,
28(2),
307–310.
Copyright 2001 by the American Geophysical Union.
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