Differences

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

--- pmip3:cmip6:design:21k:index [2015/03/27 15:58] – More changes... jypeter
+++ pmip3:cmip6:design:21k:index [2025/05/15 17:51] (current) – jypeter
@@ Line 1: / Line 1: @@
-~~DISCUSSION~~
+~~DISCUSSION:closed~~
 ====== PMIP-CMIP6 Experimental Design Discussion: Last Glacial Maximum ======
+<note warning>The PMIP4 experimental design available on the PMIP3 wiki has been **superseded** by the experimental design detailed on the [[https://pmip4.lsce.ipsl.fr/doku.php/exp_design|PMIP4 web site]]</note>
 <note tip>\\ Please submit your comments in the Discussion section at the end of this page</note>
@@ Line 34: / Line 37: @@
 **CFC** = 0
-O<sub>3</sub> = same as in CMIP5 PI
+**O<sub>3</sub>** = same as in CMIP5 PI
@@ Line 41: / Line 44: @@
 This is one of the major changes compared to pre-industrial. Prescribing the lgm ice sheets means implementing new coastlines, a new topography/bathymetry and a new ice sheet extent.
-For the modelling groups running the lgm experiment but not the deglaciation, we recommend using the PMIP3 ice sheets/coastlines, in order for simulations for PMIP3-CMIP5 and CMIP6 to be strictly comparable.
+  * Modelling groups planning to run the lgm experiment but **not the deglaciation** are advised to use the [[pmip3:design:21k:final#ice-sheets_and_related_changes|PMIP3 ice sheets/coastlines]], so that PMIP3-CMIP5 and CMIP6 can be rigorously compared.
-For the modelling groups who plan to run the deglaciation experiment (cf PMIP3 deglaciation working group), the new boundary conditions provided by Dick Peltier and Lev Tarasov can be used as well.
+  * Modelling groups planning to **run lgm as the start of the the deglaciation experiment** (cf [[pmip3:wg:degla:index|PMIP3 deglaciation working group]]) can use the new boundary conditions provided by Dick Peltier and Lev Tarasov.
@@ Line 72: / Line 75: @@
 ===== Global ocean salinity =====
-Add 1 PSU
+Add **1 PSU**.