- Timestamp:
- 2017-12-08T16:15:25+01:00 (6 years ago)
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branches/2017/dev_CNRS_2017/NEMOGCM/CONFIG/TEST_CASES/SAS_BIPER/EXP00/README
r8900 r8962 1 1 ------- 2 Context 2 Purpose 3 3 ------- 4 Th e aim of this demonstration case is to study the advection of a patch of ice in a bi-periodic channel with a slab ocean (i.e. 1 ocean layer which does not interact with sea-ice).4 This demonstration case can serve to different purposes: 5 5 6 1) The main one: study of the advection of a patch of ice in a bi-periodic channel with a slab ocean (i.e. 1 ocean layer) 7 ==> set ln_icethd=false in namelist_ice_cfg 8 9 2) Secondary: study of ice thermodynamics in the same basin 10 ==> set ln_icedyn=false in namelist_ice_cfg 11 ==> eventually change usrdef_sbc.F90 in MY_SRC to fit your needs 12 13 ----------- 14 Experiments 15 ----------- 6 16 Two experiments can be configured: 17 7 18 a) A simple channel at 3km horizontal resolution (slightly variable => +- 10%) 19 ==> remove key_agrif in cpp keys 20 8 21 b) Same as a) but with an Agrif zoom in the center 1:3, and 3 ghost cells (defined in par_oce.F90) 22 ==> add key_agrif in cpp keys 9 23 10 24 ---------- … … 13 27 Be careful, the model can only run on 1 processor in the N-S dimension 14 28 15 Compile and run the model once to get a mesh_mask.nc file with the following command (note; remove key_agrif in cpp keys for experiment a):29 a) Compile and run the model once to get a mesh_mask.nc file with the following command: 16 30 ../../../makenemo -a TEST_CASES -n SAS_BIPER -m X64_ADA -j 4 17 31 poe ./opa -procs 1 18 32 19 Create the initial condition file for sea-ice (initice.nc) by running this python script:33 b) Create the initial condition file for sea-ice (initice.nc) by running this python script: 20 34 python ./make_INITICE.py 21 35 22 Run the model a second time36 c) Run the model a second time 23 37 poe ./opa -procs 1 24 38 … … 26 40 What to look at 27 41 --------------- 28 One can test29 42 In case of purpose 1, One can test 43 --- 30 44 a) the advection scheme: Ultimate-Macho (ln_adv_UMx=T) versus Prather (ln_adv_Pra=T) 31 45 for a square (ice concentration) or a gaussian (ice volume) … … 36 50 b) the advection through an agrif zoom 1:3 37 51 52 In case of purpose 2, one can test conservation of properties: 53 --- 54 c) ice should not change at all if surface fluxes = 0 and SST = freezing temperature 55 38 56 -------------------------------------- 39 57 Interpretation of the results (remarks)
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