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pmip3:wg:degla:bc:core [2015/02/18 17:12]
ruza
pmip3:wg:degla:bc:core [2015/03/02 10:27]
ruza
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    More info here: http://​wiki.splitbrain.org/​plugin:​discussion */    More info here: http://​wiki.splitbrain.org/​plugin:​discussion */
        
-/* ~~DISCUSSION|Discussion ​on core experiment design~~ ​*+~~DISCUSSION|General discussion ​on core experiment design~~
  
 ====== Last Deglaciation Core Experiment Design ====== ====== Last Deglaciation Core Experiment Design ======
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 [[pmip3:​wg:​degla:​index|Go back]] to the main working group page. \\ [[pmip3:​wg:​degla:​index|Go back]] to the main working group page. \\
-Please note, this page is a work in progress and is not ready for discussion yet. 
  
  
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   * A **spun-up LGM** climate simulation to initialise the simulation.\\ This should have been set up as per the Last Glacial Maximum (LGM) working group requirements and recommendations.   * A **spun-up LGM** climate simulation to initialise the simulation.\\ This should have been set up as per the Last Glacial Maximum (LGM) working group requirements and recommendations.
-  * **Orbital parameters** as per [[http://​www.sciencedirect.com/​science/​article/​pii/​027737919190033Q | Berger & Loutre (1991)]]<​sup>​[1]</​sup>​. +  * **[[pmip3:​wg:​degla:​bc:​orb | Orbital parameters]]** as per [[http://​www.sciencedirect.com/​science/​article/​pii/​027737919190033Q | Berger & Loutre (1991)]]<​sup>​[1]</​sup>​. 
-  * **Greenhouse gases**: +  * **[[pmip3:​wg:​degla:​bc:​ghg | Greenhouse gases]]**: 
-      * **CO<​sub>​2</​sub>​** from [[http://​www.nature.com/​nature/​journal/​v453/​n7193/​full/​nature06949.html | Lüthi et al. (2008)]]<​sup>​[2]</​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>​. ((The high resolution [[http://​www.nature.com/​nature/​journal/​v514/​n7524/​full/​nature13799.html | Marcott et al. (2014)]]<​sup>​[4]</​sup>​ record could be used for an alternative simulation to the core, but not for the core.)) +      * **CO<​sub>​2</​sub>​** from EPICA Dome C [[http://​www.nature.com/​nature/​journal/​v453/​n7193/​full/​nature06949.html | (Lüthi et al.2008)]]<​sup>​[2]</​sup>​ on the AICC2012 timescale [[http://​www.clim-past.net/​9/​1733/​2013/​cp-9-1733-2013.html | (Veres et al.2013)]]<​sup>​[3]</​sup>​. ((The high resolution [[http://​www.nature.com/​nature/​journal/​v514/​n7524/​full/​nature13799.html | Marcott et al. (2014)]]<​sup>​[4]</​sup>​ record could be used for an alternative simulation to the core, but not for the core.)) 
-      * **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 EPICA Dome C [[http://​www.nature.com/​nature/​journal/​v453/​n7193/​full/​nature06950.html | (Loulergue et al.2008)]]<​sup>​[5]</​sup>​ on the AICC2012 timescale [[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 TALDICE ​[[http://​www.sciencedirect.com/​science/​article/​pii/​S0012821X10006023 | (Schilt et al.2010)]]<​sup>​[6]</​sup>​ on the AICC2012 timescale [[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#​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.] +  * **[[pmip3:​wg:​degla:​bc:​ice | 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.))  +  * **[[pmip3:​wg:​degla:​bc:​melt | Ice meltwater fluxes]]**: __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. For example : 
 +      * Vegetation can be fixed (to pre-industrial) or interactive 
 +      * Dust can be fixed (to pre-industrial) or prognostic ​\\ \\
  
 ==== 26-21 ka ==== ==== 26-21 ka ====
pmip3/wg/degla/bc/core.txt · Last modified: 2015/10/21 13:26 by ruza