User Tools

Site Tools


pmip3:design:6k:index

Differences

This shows you the differences between two versions of the page.

Link to this comparison view

Both sides previous revision Previous revision
Next revision
Previous revision
Next revision Both sides next revision
pmip3:design:6k:index [2009/02/06 20:34]
pasb
pmip3:design:6k:index [2009/02/10 16:27]
jypeter Cosmetic changes
Line 3: Line 3:
  
 //Go to =>// [ [[pmip3:​design:​pi:​index|PI]] ] - [ [[pmip3:​design:​21k:​index|21ka]] ] - [ [[pmip3:​design:​lm:​index|LM]] ] //Go to =>// [ [[pmip3:​design:​pi:​index|PI]] ] - [ [[pmip3:​design:​21k:​index|21ka]] ] - [ [[pmip3:​design:​lm:​index|LM]] ]
-====== 6ka Experimental Design ====== 
  
  
-<note warning>%%  ​Page in progress : this is not the final versionUse the discussion ​pannel ​below for comments%%</​note>​+====== 6ka Experimental Design ====== 
 + 
 +<note warning>**Page in progress**: this is not the final version\\ \\ Use the discussion ​panel below for comments</​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 ​ ^  Alternative solution ​ 
-|  ​date of the Vernal ​equinox ​ |  March 21 at Noon  | | +|  Orbital parameters ​ |  **ecc** = 0.018682\\   **obl** = 24.105°\\ ​  **peri-180°** = 0.87°  | | 
-|  Trace Gazes  ​| ​ **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  | |+|  ​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  | |
 |  Aerosols ​ |  Same as PI  | | |  Aerosols ​ |  Same as PI  | |
 |    | |  | |    | |  |
 |  Solar constant ​ |  1365W/​m<​sup>​2</​sup> ​ |  As in PI  | |  Solar constant ​ |  1365W/​m<​sup>​2</​sup> ​ |  As in PI  |
 |  Vegetation ​    ​| ​ Interactive ​ |  See specific note below | |  Vegetation ​    ​| ​ Interactive ​ |  See specific note below |
-|  Ice sheet      ​|  ​remnant ​Laurentide ice-sheet (provided) ​ |  Same as PI  | +|  Ice sheets ​     ​|  ​Remnant ​Laurentide ice-sheet (provided) ​ |  Same as PI  | 
-|  Topography and coastline ​ ​| ​ Modification of the Hudson Bay (provided) ​ |  Same as PI  |+|  Topography and coastlines ​ ​| ​ Modification of Hudson Bay coastlines ​(provided) ​ |  Same as PI  |
  
  
-** Vegetation ​ **+==== Vegetation ​==== 
 Depending on the complexity of the model used the vegetation will be either \\ Depending on the complexity of the model used the vegetation will be either \\
 +
 - computed by the model \\ - computed by the model \\
 - prescribed to PI (some ESM may only compute vegetation phenology and carbon cycle)\\ - 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) \\ - 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 ) +- Obtained from asynchronous ​coupling with a DVGM (Biome 4 model provided) ​ 
 + 
 + 
 +==== For Earth System Models with interactive carbone cycle ==== 
 + 
 +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]])
  
-** For Earth System Model with interactive carbone cycle ** 
-The simlations are force by the CO2 concentrations. Please use the same protocal 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 carefuly using the following tables ​ 
  
  
Line 42: Line 50:
 ===== Initial conditions ===== ===== Initial conditions =====
  
-^  ^ PMIP3 ^ Alternative solution ^ +^  ^  PMIP3   Alternative solution ​ 
-| Initial conditions |  ​branch ​off PI after adjustement | Same as in PI | +| Initial conditions |  ​Branch ​off PI after adjustement ​ | Same as in PI | 
-| Model spin up      |  Same as in PI |  |+| Model spin up      |  Same as in PI  |  |
  
  
pmip3/design/6k/index.txt · Last modified: 2010/09/16 12:35 by jypeter