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pmip3:wg:degla:bc:core

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Last Deglaciation Core Experiment Design

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Please note, this page is a work in progress and is not ready for discussion yet.


Proposal

Following wide consultation over the past year, this is our first-draft proposal for the last deglaciation core simulation.
Please use the Discussion section below to comment on general aspects of the proposal and make suggestions for amendments.

For comments on specific boundary conditions, please use the Discussion sections on their dedicated pages:


21-9 ka

All core simulations must span this time-period. Use:

26-21 ka

For those who wish to begin their simulation from before the PMIP LGM, use:

  • Orbit as per Berger & Loutre (1991)[1] for this time period.
  • All other boundary conditions as per the PMIP LGM Working Group.


Points To Discuss

Please think about the following points and add any comments on these or any other aspects of the experiment design to the discussion section below: [Topics will be added here as they are raised below or by email.]

  • No specific points yet.


References

  1. Berger, A. & Loutre, M. F. Insolation values for the climate of the last 10 million years. Quat. Sci. Rev. 10, 297–317 (1991).
  2. Lüthi, D. et al. High-resolution carbon dioxide concentration record 650,000–800,000 years before present. Nature 453, 379–382 (2008).
  3. Veres, D. et al. The Antarctic ice core chronology (AICC2012): an optimized multi-parameter and multi-site dating approach for the last 120 thousand years. Clim Past 9, 1733–1748 (2013).
  4. Marcott, S. A. et al. Centennial-scale changes in the global carbon cycle during the last deglaciation. Nature 514, 616–619 (2014).
  5. Loulergue, L. et al. Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 years. Nature 453, 383–386 (2008).
  6. Schilt, A. et al. Atmospheric nitrous oxide during the last 140,000 years. Earth Planet. Sci. Lett. 300, 33–43 (2010).
  7. Argus, D. F., Peltier, W. R., Drummond, R. & Moore, A. W. The Antarctica component of postglacial rebound model ICE-6G_C (VM5a) based on GPS positioning, exposure age dating of ice thicknesses, and relative sea level histories. Geophys. J. Int. ggu140 (2014).
  8. Peltier, W. R., Argus, D. F. & Drummond, R. Space geodesy constrains ice age terminal deglaciation: The global ICE-6G_C (VM5a) model. J. Geophys. Res. Solid Earth 2014JB011176 (2015).


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1)
The high resolution Marcott et al. (2014)[4] record could be used for an alternative simulation to the core, but not for the core.
2)
Global meltwater fluxes that are consistent with the ice sheet reconstructions will be provided for alternative simulations to the core, but must not be used for the core.

General discussion on core experiment design

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pmip3/wg/degla/bc/core.1424263502.txt.gz · Last modified: 2015/02/18 12:45 by ruza