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005        20171030123209.0
006        m^^^^^o^^d^^^^^^^^
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245 00 |a Transient Simulation of Last Deglaciation with a New Mechanism for Bolling-Allerod Warming |h [electronic resource].
260        |a [S.l.] : |b American Association for the Advancement of Science, |c 2009.
490        |a Science Magazine.
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 We conducted the first synchronously coupled atmosphere-ocean general circulation model simulation from the Last Glacial Maximum to the Bølling-Allerød (BA) warming. Our model reproduces several major features of the deglacial climate evolution, suggesting a good agreement in climate sensitivity between the model and observations. In particular, our model simulates the abrupt BA warming as a transient response of the Atlantic meridional overturning circulation (AMOC) to a sudden termination of freshwater discharge to the North Atlantic before the BA. In contrast to previous mechanisms that invoke AMOC multiple equilibrium and Southern Hemisphere climate forcing, we propose that the BA transition is caused by the superposition of climatic responses to the transient CO2 forcing, the AMOC recovery from Heinrich Event 1, and an AMOC overshoot.
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.
600        |a. |y last glacial maximum
600        |a. |z Southern Hemisphere
650        |a climate change.
651        |a Atlantic Region.
700        |a Z. Liu.
700        |a B.L. Otto-Bliesner.
700        |a F. He.
700        |a E.C. Brady.
700        |a R. Tomas.
700        |a P.U. Clark.
700        |a A. E. Carlson.
700        |a J. Lynch- Stieglitz.
700        |a W. Curry.
700        |a E. Brook.
700        |a D. Erickson.
700        |a R. Jacob.
700        |a J. Kutzbach.
700        |a J. Cheng.
773 0    |t Transient Simulation of Last Deglaciation with a New Mechanism for Bolling-Allerod Warming
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/FI15052525/00001 |y Click here for full text
856 42 |3 FULL TEXT- Transient Simulation of Last Deglaciation with a New Mechanism for Bolling-Allerod Warming |u http://science.sciencemag.org/content/325/5938/310.full |y Transient Simulation of Last Deglaciation with a New Mechanism for Bolling-Allerod Warming
992 04 |a http://dpanther.fiu.edu/sobek/content/FI/15/05/25/25/00001/FI15052525_thm.jpg
997        |a Sea Level Rise


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