Sea-level rise due to polar ice-sheet mass loss during past warm periods-Reference-Cited by-同舟云学术

Sea-level rise due to polar ice-sheet mass loss during past warm periods

Published:2015-07-10 Issue:6244 Volume:349 Page:
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Dutton A.¹,Carlson A. E.²,Long A. J.³,Milne G. A.⁴,Clark P. U.²,DeConto R.⁵,Horton B. P.⁶⁷,Rahmstorf S.⁸,Raymo M. E.⁹

Affiliation:

1. Department of Geological Sciences, University of Florida,Gainesville, FL 32611, USA.

2. College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA.

3. Department of Geography, Durham University, Durham, UK.

4. Department of Earth Sciences, University of Ottawa, Ottawa, Canada.

5. Department of Geosciences, University of Massachusetts, Amherst, MA 01003, USA.

6. Department of Marine and Coastal Sciences, Rutgers University, New Brunswick, NJ 08901, USA.

7. Earth Observatory of Singapore, Nanyang Technological University, Singapore, 639798.

8. Potsdam Institute for Climate Impact Research, Potsdam, Germany.

9. Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY 10964, USA.

Abstract

Warming climate, melting ice, rising seas We know that the sea level will rise as climate warms. Nevertheless, accurate projections of how much sea-level rise will occur are difficult to make based solely on modern observations. Determining how ice sheets and sea level have varied in past warm periods can help us better understand how sensitive ice sheets are to higher temperatures. Dutton et al. review recent interdisciplinary progress in understanding this issue, based on data from four different warm intervals over the past 3 million years. Their synthesis provides a clear picture of the progress we have made and the hurdles that still exist. Science , this issue 10.1126/science.aaa4019

Funder

NSF

Natural Environment Research Council

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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