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pmip3:wg:degla:bc:core [2015/02/18 14:01]
ruza
pmip3:wg:degla:bc:core [2015/02/18 17:12]
ruza
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 ==== 21-9 ka ==== ==== 21-9 ka ====
  
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       * **CH<​sub>​4</​sub>​** from [[http://​www.nature.com/​nature/​journal/​v453/​n7193/​full/​nature06950.html | Loulergue et al. (2008)]]<​sup>​[5]</​sup>​ on the AICC2012 timescale of [[http://​www.clim-past.net/​9/​1733/​2013/​cp-9-1733-2013.html | Veres et al. (2013)]]<​sup>​[3]</​sup>​.       * **CH<​sub>​4</​sub>​** from [[http://​www.nature.com/​nature/​journal/​v453/​n7193/​full/​nature06950.html | Loulergue et al. (2008)]]<​sup>​[5]</​sup>​ on the AICC2012 timescale of [[http://​www.clim-past.net/​9/​1733/​2013/​cp-9-1733-2013.html | Veres et al. (2013)]]<​sup>​[3]</​sup>​.
       * **N<​sub>​2</​sub>​O** from [[http://​www.sciencedirect.com/​science/​article/​pii/​S0012821X10006023 | Schilt et al. (2010)]]<​sup>​[6]</​sup>​ on the AICC2012 timescale of [[http://​www.clim-past.net/​9/​1733/​2013/​cp-9-1733-2013.html | Veres et al. (2013)]]<​sup>​[3]</​sup>​.       * **N<​sub>​2</​sub>​O** from [[http://​www.sciencedirect.com/​science/​article/​pii/​S0012821X10006023 | Schilt et al. (2010)]]<​sup>​[6]</​sup>​ on the AICC2012 timescale of [[http://​www.clim-past.net/​9/​1733/​2013/​cp-9-1733-2013.html | Veres et al. (2013)]]<​sup>​[3]</​sup>​.
-  * **Ice sheets**: Choice of either the [[pmip3:​wg:​degla:​bc:​ice#​ice6g_c_reconstruction ​ICE6G_C]]<​sup>​[7-8]</​sup>​ or [[pmip3:​wg:​degla:​bc:​ice#​lev_tarasov_s_reconstruction | Lev Tarasov'​s]]<​sup>​[9-12]</​sup>​ global reconstruction of ice sheet evolution. \\ Whichever is chosen for the LGM should be kept for the whole simulation. \\ [See the [[pmip3:​wg:​degla:​bc:​ice | last deglaciation ice sheets]] page for more information on the ice sheets.]+  * **Ice sheets**: Choice of either the [[pmip3:​wg:​degla:​bc:​ice#​ice-6g_c_reconstruction ​ICE-6G_C]]<​sup>​[7-8]</​sup>​ or [[pmip3:​wg:​degla:​bc:​ice#​lev_tarasov_s_reconstruction | Lev Tarasov'​s]]<​sup>​[9-12]</​sup>​ global reconstruction of ice sheet evolution. \\ Whichever is chosen for the LGM should be kept for the whole simulation. \\ [See the [[pmip3:​wg:​degla:​bc:​ice | last deglaciation ice sheets]] page for more information on the ice sheets.]
   * **Meltwater**:​ __no meltwater__ in the core. ((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.)) ​   * **Meltwater**:​ __no meltwater__ in the core. ((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.)) ​
   * Other boundary conditions: keep as per the LGM. \\ \\   * Other boundary conditions: keep as per the LGM. \\ \\
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-===== Points ​To Discuss ​=====+===== 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.] 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.]
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-=====References=====+===== References =====
   - Berger, A. & Loutre, M. F. Insolation values for the climate of the last 10 million years. Quat. Sci. Rev. 10, 297–317 (1991).   - Berger, A. & Loutre, M. F. Insolation values for the climate of the last 10 million years. Quat. Sci. Rev. 10, 297–317 (1991).
   - Lüthi, D. et al. High-resolution carbon dioxide concentration record 650,​000–800,​000 years before present. Nature 453, 379–382 (2008).   - Lüthi, D. et al. High-resolution carbon dioxide concentration record 650,​000–800,​000 years before present. Nature 453, 379–382 (2008).
pmip3/wg/degla/bc/core.txt · Last modified: 2015/10/21 13:26 by ruza