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Kinematic Constraints on Glacier Contributions to 21st-Century Sea-Level Rise
W. T. Pfeffer,1*J. T. Harper,2S. O'Neel3
On the basis of climate modeling and analogies with past conditions,the potential for multimeter increases in sea level by the endof the 21st century has been proposed. We consider glaciologicalconditions required for large sea-level rise to occur by 2100and conclude that increases in excess of 2 meters are physicallyuntenable. We find that a total sea-level rise of about 2 metersby 2100 could occur under physically possible glaciologicalconditions but only if all variables are quickly acceleratedto extremely high limits. More plausible but still acceleratedconditions lead to total sea-level rise by 2100 of about 0.8meter. These roughly constrained scenarios provide a "most likely"starting point for refinements in sea-level forecasts that includeice flow dynamics.
1 Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO 80309, USA. 2 Department of Geosciences, University of Montana, Missoula, MT 59812, USA. 3 Scripps Institution of Oceanography, University of California San Diego, San Diego, CA 92093, USA.
* To whom correspondence should be addressed. E-mail: pfeffer{at}tintin.colorado.edu
From the Cover: Assessing dangerous climate change through an update of the Intergovernmental Panel on Climate Change (IPCC) "reasons for concern".
J. B. Smith, S. H. Schneider, M. Oppenheimer, G. W. Yohe, W. Hare, M. D. Mastrandrea, A. Patwardhan, I. Burton, J. Corfee-Morlot, C. H. D. Magadza, et al. (2009)
PNAS
106, 4133-4137
|Abstract »|Full Text »|PDF »
Irreversible climate change due to carbon dioxide emissions.
S. Solomon, G.-K. Plattner, R. Knutti, and P. Friedlingstein (2009)
PNAS
106, 1704-1709
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Sea levels: science and society.
R. Edwards (2008)
Progress in Physical Geography
32, 557-574
|PDF »