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|a The sea-level conundrum |h [electronic resource] |b case studies from palaeo-archives |y English. |
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|a [S.l.] : |b John Wiley & Sons, Ltd., |c 2010. |
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|a Journal of Quaternary Science. |
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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 Uncertainties in sea-level projections for the 21st century have focused ice sheet
modelling efforts to include the processes that are thought to be contributing to the recently observed
rapid changes at ice sheet margins. This effort is still in its infancy, however, leaving us unable to make
reliable predictions of ice sheet responses to a warming climate if such glacier accelerations were to
increase in size and frequency. The geological record, however, has long identified examples of
nonlinear ice sheet response to climate forcing (Shackleton NJ, Opdyke ND. 1973. Oxygen isotope
and paleomagnetic stratigraphy of equatorial Pacific core V28–239, late Pliocene to latest Pleistocene.
Geological Society of America Memoirs 145: 449–464; Fairbanks RG. 1989. A 17,000 year glacioeustatic
sea level record: influence of glacial melting rates on the Younger Dryas event and deep ocean
circulatio |
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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 PALeo SEA level working group. |
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|t The sea-level conundrum |
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|a dpSobek |c Sea Level Rise |
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|u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15061833/00001 |y Click here for full text |
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|3 Host material |u http://onlinelibrary.wiley.com/doi/10.1002/jqs.1270/epdf |y The sea-level conundrum |
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|a http://dpanther.fiu.edu/sobek/content/FI/15/06/18/33/00001/PALSEA_(PALeo SEA level working group)_2010_The sea-level conundrumthm.jpg |
