Ice-Sheet and Sea-Level Changes-Reference-Cited by-同舟云学术

Ice-Sheet and Sea-Level Changes

Published:2005-10-21 Issue:5747 Volume:310 Page:456-460
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Alley Richard B.¹²³⁴⁵,Clark Peter U.¹²³⁴⁵,Huybrechts Philippe¹²³⁴⁵,Joughin Ian¹²³⁴⁵

Affiliation:

1. Department of Geosciences and Earth and Environmental Systems Institute, Pennsylvania State University, Deike Building, University Park, PA 16802, USA.

2. Department of Geosciences, Oregon State University, Corvallis, OR 97331, USA.

3. Alfred-Wegener-Institut für Polar- und Meeresforschung, Postfach 120161, D-27515 Bremerhaven, Germany.

4. Departement Geografie, Vrije Universiteit Brussel, Pleinlaan 2, B-1050 Brussel, Belgium.

5. Polar Science Center, Applied Physics Lab, University of Washington, 1013 NE 40th Street, Seattle, WA 98105, USA.

Abstract

Future sea-level rise is an important issue related to the continuing buildup of atmospheric greenhouse gas concentrations. The Greenland and Antarctic ice sheets, with the potential to raise sea level ∼70 meters if completely melted, dominate uncertainties in projected sea-level change. Freshwater fluxes from these ice sheets also may affect oceanic circulation, contributing to climate change. Observational and modeling advances have reduced many uncertainties related to ice-sheet behavior, but recently detected, rapid ice-marginal changes contributing to sea-level rise may indicate greater ice-sheet sensitivity to warming than previously considered.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference69 articles.

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