Nemo
Welcome to the Bristol Nemo Page!
Here are a few tips and comments based on Bristol's experiences compiling and running NEMO. Hopefully, you will find some useful.
Please take a look the official NEMO webpage before continuing with this page.
Projects using Nemo at Bristol
Mediterranean Sea
Amundsen Sea
Thinning of the Pine Island Glacier, West Antarctica, has been observed during the 1990s. It has been suggested that relatively warm water at the base of the ice shelf has triggered the thinning. The source of and mechanism driving this warm water is unknown.
We are constructing a regional model of the Amunsden Sea using Nemo to investigate ocean circulation close to Pine Island Bay. Input data at the sea surface and at the open boundaries are constructed using output data from the OCCAM global ocean model.
ORCA2_LIM test case
Nemo provides a test case, ORCA2_LIM, for a global ocean run coupled with the sea-ice model. The run simulates one year.
The configuration for ORCA2_LIM is downloaded through CVS when getting Nemo and the necessary forcing files are provided through a link on the Nemo website.
Region model
How to set up a regional model starting from the ORCA2_LIM test case:
- Create a new configuration for the regional model.
- In directory modipsl/config/ create a new directory AMUNDSEN, for example, and copy the contents of the ORCA2_LIM directory into AMUNDSEN.
- Edit file fait_config in modipsl/modeles/UTIL/. Add
\n AMUNDSEN
toLIST =
and add the lineset -A DIR_AMUNSDEN OPA_SRC C1D_SRC NST_SRC
.
- Change CPP keys by editing BB_make.ldef in modipsl/config/AMUNDSEN/scripts/. Remove
key_orca_r2
since you're not running a global model and addkey_obc
to invoke open boundary conditions instead. - TIP: modify tradmp.F90 in modipsl/modeles/NEMO/OPA_SRC/TRA/. Replace the line
if (cp_cfg=="orca" .AND. (ndmp > 0 .OR. ndmp==-1)) then
withif (ndmp > 0 .OR. ndmp==-1) then
. If you don't make the change you'll get the error messagetra_dmp: You should not have seen this print error?
. With this change you can apply tracer damping as in the ORCA configurations (i.e. global models for various resolutions) without special treatment for particular areas such as the Meditarrean
Open boundary conditions
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