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pmip3:design:6k:index [2009/02/10 13:45]
masa
pmip3:design:6k:index [2010/09/16 12:35]
jypeter Added link to final BC page in the top warning
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 ~~ODT~~ ~~ODT~~
-~~DISCUSSION~~+~~DISCUSSION:closed~~
  
-//Go to =>// [ [[pmip3:​design:​pi:​index|PI]] ] - [ [[pmip3:​design:​21k:​index|21ka]] ] - [ [[pmip3:​design:​lm:​index|LM]] ]+<​html><​a name="​page_top_tag">&​nbsp</​a></​html>​ 
 +//Go to =>// [ [[pmip3:​design:​pi:​index|PI]] ​] - [ **6ka** ​] - [ [[pmip3:​design:​21k:​index|21ka]] ] - [ [[pmip3:​design:​lm:​index|LM]] ] - [ [[pmip3:​design:​8k2:​index|8.2ka]] ] - [ [[pmip3:​design:​li:​index|LI]] ] - [ [[pmip3:​design:​plio:​index|Plio]] ]
  
  
 ====== 6ka Experimental Design ====== ====== 6ka Experimental Design ======
  
-<note warning>**Page in progress**: this is not the final version\\ \\ Use the discussion pannel below for comments</​note>​+<note warning>This was a BC //​development page// (see [[index#​page_bottom_tag|discussion]] panel at the end of the page)\\ \\ Make sure you use the [[pmip3:​design:​6k:​final|final version of the 6k BC]]!</​note>​ 
 ===== Boundary conditions ===== ===== Boundary conditions =====
  
-**Summary of 6ka boundary conditions ​**+==== Summary of 6ka boundary conditions ​====
  
-^      ^   ​PMIP3 ​ ^  ​Alternative ​solution ^ + 
-|  Orbital parameters ​ |  **ecc**=0.018682,   **obl**=24.105°,   **peri-180°**= 0.87° ​ | |+^      ^   PMIP3/​CMIP5 ​ ​^  ​Minimum ​solution ​ 
 +|  Orbital parameters ​ |  ​**ecc** = 0.018682 ​] - [ **obl** = 24.105° ​] - [ **peri-180°** = 0.87° ​ ​| ​ |
 |  Date of vernal equinox ​ |  March 21 at noon  | | |  Date of vernal equinox ​ |  March 21 at noon  | |
-|  Trace gases  |  **CO<​sub>​2</​sub>​** = 280 ppm**CH<​sub>​4</​sub>​** = 650 ppb**N<​sub>​2</​sub>​O** = 270 ppb**CFC** = 0**O<​sub>​3</​sub>​** = same as PI  | |+|  Trace gases  |  ​**CO<​sub>​2</​sub>​** = 280 ppm ] - [ **CH<​sub>​4</​sub>​** = 650 ppb ] - [ **N<​sub>​2</​sub>​O** = 270 ppb ] - [ **CFC** = 0 ] - [ **O<​sub>​3</​sub>​** = same as PI  | |
 |  Aerosols ​ |  Same as PI  | | |  Aerosols ​ |  Same as PI  | |
 |    | |  | |    | |  |
-|  Solar constant ​ |  ​1365W/​m<​sup>​2</​sup> ​ |  As in PI  | +|  Solar constant ​ |  ​1365 W/​m<​sup>​2</​sup> ​ |  As in PI  | 
-|  Vegetation ​    ​|  ​Interactive ​ ​| ​ See specific note below +|  Vegetation ​    ​|  ​prescribed or interactive as in CMIP5 PI  ​| ​   
-|  Ice sheets ​     |  Remnant Laurentide ice-sheet (provided) ​ |  Same as PI  | +|  Ice sheets ​     |  Remnant Laurentide ice-sheet (provided*)  |  Same as PI  | 
-|  Topography and coastlines ​ |  Modification of Hudson Bay coastlines (provided) ​ |  Same as PI  |+|  Topography and coastlines ​ |  Modification of Hudson Bay coastlines (provided*)  |  Same as PI  |
  
 +*For the ice-sheet reconstruction,​ see discussion on LGM wiki page
  
-** Vegetation  ​**+Please use the [[index#​page_bottom_tag|discussion]] panel to **comment** this table!
  
-Depending on the complexity of the model used the vegetation will be either \\ 
  
-- computed by the model \\ +==== Vegetation ====
-- prescribed to PI (some ESM may only compute vegetation phenology and carbon cycle)\\ +
-- prescribed to 6ka vegetation reconstructed from a combination of model output and data analyses (please use the map provided here) \\ +
-- Obtained from asynschonous coupling with a DVGM (Biome 4 model provided) ​+
  
 +The vegetation should be treated as in the CMIP5 PI experiment. The reason is that in CMIP5 we test the version of the model used for future climate projections. Since OA and ESM models will be considered, depending on the model used the vegetation will be 
  
-** For Earth System Models ​with interactive carbone cycle **+  ​prescribed to PI (which means both vegetation types and LAI are prescribed ) 
 +  ​Prescribed to PI with interactive LAI (models ​with interactive carbone cycle, but no vegetation dynamics) 
 +  ​Computed by the model (models with dynamic vegetation) ​
  
-The simulations ​are forced by CO2 concentrations. Please use the same protocal as in CMIP5 to store the carbone fluxes ​and the variables ​needed for PCMIP (see list here+There are still questions concerning ​the possibility ​to have a 6ka reconstructed vegetation from a combination of model output ​and data analyses that could be used for sensitivity experiments. Please tell if you are interested by such a map and what would be the best variables ​(pft?) that should be provided ​(see comment from B. Otto-Bliesner in the discussion pannel).  ​
  
-** Insolation **+==== For Earth System Models with interactive carbone cycle ====
  
-Note that insolation should follows PMIP requirements. Please ​check it carefuly using the following tables ​([[http://​pmip2.lsce.ipsl.fr/​design/​tables/​inso_tables_6k.shtml|6ka BP insolation tables]])+The simulations are forced by CO2 concentrations. Please ​use the same protocol as in CMIP5 to store the carbone fluxes and the variables needed for PCMIP (see list here
  
 +==== Insolation ====
  
 +Note that insolation should follows PMIP requirements. Please check it carefully using the following tables ([[http://​pmip2.lsce.ipsl.fr/​design/​tables/​inso_tables_6k.shtml|6ka BP insolation tables]])
  
  
  
-===== Initial conditions ===== 
  
-^  ^ PMIP3 ^ Alternative solution ^ 
-| Initial conditions |  branch off PI after adjustement | Same as in PI | 
-| Model spin up      |  Same as in PI |  | 
  
 +===== Initial conditions =====
 +
 +^  ^  PMIP3  ^  Alternative solution ​ ^
 +| Initial conditions |  Branch off PI after adjustement ​ |  Same as in PI  |
 +| Model spin up      |  Same as in PI  |  |
  
  
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pmip3/design/6k/index.txt · Last modified: 2010/09/16 12:35 by jypeter