LDR   02790nam^^22003253a^4500
001        FI15061870_00001
005        20160129134829.0
006        m^^^^^o^^d^^^^^^^^
007        cr^^n^---ma^mp
008        150707n^^^^^^^^xx^||||^o^^^^^|||^u^eng^d
245 00 |a The Role of Ocean Thermal Expansion in Last Interglacial Sea Level Rise |h [electronic resource].
260        |c 2011.
506        |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.
520 3    |a A compilation of paleoceanographic data and a coupled atmosphere-ocean climate model were used to examine global ocean surface temperatures of the Last Interglacial (LIG) period, and to produce the first quantitative estimate of the role that ocean thermal expansion likely played in driving sea level rise above present day during the LIG. Our analysis of the paleoclimatic data suggests a peak LIG global sea surface temperature (SST) warming of 0.7±0.6°C compared to the late Holocene. Our LIG climate model simulation suggests a slight cooling of global average SST relative to preindustrial conditions (ΔSST = -0.4°C), with a reduction in atmospheric water vapor in the Southern Hemisphere driven by a northward shift of the Intertropical Convergence Zone, and substantially reduced seasonality in the Southern Hemisphere. Taken together, the model and paleoceanographic data imply a minimal contribution of ocean thermal expansion to LIG sea level rise above present day. Uncertainty remains, but it seems unlikely that thermosteric sea level rise exceeded 0.4±0.3 m during the LIG. This constraint, along with estimates of the sea level contributions from the Greenland Ice Sheet, glaciers and ice caps, implies that 4.1 to 5.8 m of sea level rise during the Last Interglacial period was derived from the Antarctic Ice Sheet. These results reemphasize the concern that both the Antarctic and Greenland Ice Sheets may be more sensitive to temperature than widely thought.
533        |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.
650    0 |a Climate Change.
650    0 |a Sea Level Rise.
650    0 |a Global Warming.
650    0 |a Ocean.
720 1    |a McKay, Nicholas P..
720 1    |a Overpeck, Jonathan T..
720 1    |a Otto-Bliesner, Bette L..
773 0    |t The Role of Ocean Thermal Expansion in Last Interglacial Sea Level Rise
830    0 |a dpSobek.
830    0 |a Sea Level Rise.
852        |a dpSobek |c Sea Level Rise
856 40 |u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15061870/00001 |y Click here for full text
856 42 |3 Host material |u http://onlinelibrary.wiley.com/doi/10.1029/2011GL048280/abstract |y The Role of Ocean Thermal Expansion in Last Interglacial Sea Level Rise
992 04 |a http://dpanther.fiu.edu/sobek/content/FI/15/06/18/70/00001/FI15061870thm.jpg
997        |a Sea Level Rise


The record above was auto-generated from the METS file.