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Cited by 846

The DOI matches its Crossref record; 138 of the 138 references it cites were found in a registry or an index.

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

Open access
Dutton, A., Carlson, A. E., Long, A. J., Milne, G. A., Clark, P. U., DeConto, R., Horton, B. P., Rahmstorf, S., Raymo, M. E.·2015·Science

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

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Crossref · 10.1126/science.aaa4019

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Metadata

Authors
Dutton, A., Carlson, A. E., Long, A. J., Milne, G. A., Clark, P. U., DeConto, R., Horton, B. P., Rahmstorf, S., & Raymo, M. E.
Venue
Science
Published
2015-07-10
Volume
349
Issue
6244
Pages
aaa4019-aaa4019
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W1733916393
Cited by
846
References
138
FWCI
47.19
Type
journal article
Language
en
Open access
green

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Bibliographic data: Semantic Scholar, OpenAlex, Crossref.

Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.