This shows you the differences between two versions of the page.
Both sides previous revision Previous revision Next revision | Previous revision Next revision Both sides next revision | ||
pmip3:cmip6:design:21k:index [2015/03/24 21:51] masa |
pmip3:cmip6:design:21k:index [2015/03/24 21:59] masa |
||
---|---|---|---|
Line 1: | Line 1: | ||
- | ~~DISCUSSION~~ | ||
- | |||
- | ====== PMIP-CMIP6 Experimental Design Discussion: Last Glacial Maximum ====== | ||
- | |||
- | <note tip>\\ Please submit your comments in the Discussion section at the end of this page</note> | ||
- | |||
~~DISCUSSION~~ | ~~DISCUSSION~~ | ||
Line 64: | Line 58: | ||
We invite the modelling groups planning to run simulations with an interactive dust cycle to comment on the most appropriate methodology for their model, in particular as to their ability to use a interactive vegetation description. | We invite the modelling groups planning to run simulations with an interactive dust cycle to comment on the most appropriate methodology for their model, in particular as to their ability to use a interactive vegetation description. | ||
- | ** A note | + | ** A note on the fresh water budget ** |
+ | |||
+ | Modelling groups are advised to carefully check the fresh water budget in their lgm experiments in order to avoid unnecessary drifts of the ocean salinity. It can be necessary to route the snow which has fallen in excess on the ice sheets to the ocean. Given the change in coastlines, it is also sometimes necessary relocate the large rivers' estuaries on the coast. | ||
+ | |||
+ | ** Glocal ocean salinity ** | ||
+ | Add 1PSU | ||