Differences

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

--- pmip3:design:6k:final [2010/02/05 13:33] – jypeter
+++ pmip3:design:6k:final [2015/03/02 10:48] (current) – Removed the sentence about the (non existing) 6k vegetation map jypeter
@@ Line 1: / Line 1: @@
 <html><a name="page_top_tag">&nbsp</a></html>
-//Go to =>// [ [[pmip3:design:pi:final|PI]] ] - [ **6ka** ] - [ [[pmip3:design:21k:final|21ka]] ] - [ [[pmip3:design:lm:final|LM]] ]
+//Go to =>// [ [[pmip3:design:pi:final|PI]] ] - [ **6ka** ] - [ [[pmip3:design:21k:final|21ka]] ] - [ [[pmip3:design:lm:final|LM]] ] & Non-CMIP5 exps: [ [[pmip3:design:li:final|LI]] ]
 ====== 6ka Experimental Design ======
@@ Line 28: / Line 28: @@
   * 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)
-A 6ka reconstructed vegetation map from a combination of model outputs and data analyses will be provided for sensitivity experiments. If you are interested please contact Bette Otto-Bliesner, Sandy Harrison and Pat Bartlein who will lead the corresponding working group.
 ==== For Earth System Models with interactive carbon cycle ====
@@ Line 42: / Line 40: @@
 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]])
-Check carefully the date of the Vernal equinox, because it has implications to compare paleo and PI seasonal cycle
+Check carefully the date of the Vernal equinox, because it has implications when we compare paleo and PI seasonal cycle
 ==== 6ka  for groups only running PMIP3 experiments ====