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|a Paleoclimatic Evidence for Future Ice-Sheet Instability and Rapid Sea-Level Rise |h [electronic resource] |y English. |
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|a [S.l.] : |b American Association for the Advancement of Science, |c 2006. |
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|a Science Magazine Volume 311, 1747. |
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|a Please contact the owning institution for licensing and permissions. It is the user's responsibility to ensure use does not violate any third party rights. |
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|a Sea-level rise from melting of polar ice sheets is one of the largest potential threats of future
climate change. Polar warming by the year 2100 may reach levels similar to those of 130,000 to
127,000 years ago that were associated with sea levels several meters above modern levels; both
the Greenland Ice Sheet and portions of the Antarctic Ice Sheet may be vulnerable. The record of
past ice-sheet melting indicates that the rate of future melting and related sea-level rise could be
faster than widely thought. |
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|a Electronic reproduction. |c Florida International University, |d 2015. |f (dpSobek) |n Mode of access: World Wide Web. |n System requirements: Internet connectivity; Web browser software. |
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|a Overpeck, Jonathan T.. |
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|a Otto-Bliesner, Bette L.. |
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|t Paleoclimatic Evidence for Future Ice-Sheet Instability and Rapid Sea-Level Rise |
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|a dpSobek |c Sea Level Rise |
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|u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15061835/00001 |y Click here for full text |
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|3 FULL TEXT- Paleoclimatic Evidence for Future Ice-Sheet Instability and Rapid Sea-Level Rise |u http://science.sciencemag.org/content/311/5768/1747 |y Paleoclimatic Evidence for Future Ice-Sheet Instability and Rapid Sea-Level Rise |
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|a http://dpanther.fiu.edu/sobek/content/FI/15/06/18/35/00001/Overpeck et al_2006_Paleoclimatic Evidence for Future Ice-Sheet Instability and Rapid Sea-Level Rise |
