wiki:Bathy

Version 1 (modified by nbouttes, 3 years ago) (diff)

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Bathymetry


1. Bathy

Things to modify

2.1. With new bathymetry

1) Modify / check choixcomposantes.h in scenario (scenario/deglaciation_pmip4_P_T/sources-2tr or scenario/deglaciation_pmip4_P_T/sources-17tr):

BATHY 2 
F_PALAEO 3 
ISM 3 
SMB_TYP 1 
CPLTYP 1 
DOWNSTS 1 
DOWNSCALING 1
LGMSWITCH 0 


Note: to have uncorrected FWF from ice sheets on top (not to be done in equilibrirum runs, only transient, otherwise issue with salinity computation):

APPLY_UNCORFWF 1
F_PALAEO_FWF 1 

Note 2: to have corrected FWF from ice sheets on top:

APPLY_UNCORFWF 0
F_PALAEO_FWF 1

2) Specifify the date in ludus-code/ecbilt/parameters/palaeo_transient_parameters.dat (see LGM section earlier).

3) Choose the correct ice sheet reconstruction for topography in ludus-code/ecbilt/inputdata/

  • For Peltier: ICE6G_26k-0k_hemin40_Aurelien.nc:

ln -s ICE6G_26k-0k_hemin40_Aurelien.nc Gano_40k-0k_hemin40.nc
This file has 105 time slices, with a time step of 250 years, the first time slice is 26k and the last one is 0.

  • For Tarasov: GLAC1D_26k-0k_hemin40_Aurelien.nc

ln -s GLAC1D_26k-0k_hemin40_Aurelien.nc Gano_40k-0k_hemin40.nc
This file has 261 time slices, with a time step of 100 years, the first time slice is 26k and the last one is 0.

You will also need to modify in palaeo_timer_mod.f90 and input_subgrid2L.f90 the values of :

  • nb_steps_fism
  • update_time_fism
  • time_max_fism

4) In ludus-code/lbm/sources/routageEAU.f90: bricole_caspienne=.FALSE.

5) Change the path for GRISLI: in config/grisli.path change the line for:
/home/acclimate/aquiquet/GRISLI/GRISLI_iLoveclim

6) If you want to use berg.nc instead of berg.dat (for ice sheets also in SO):
/ecbilt_clio/global_flags/BC_switches.h

7) Specify inputdata, sources and restart (here starting from LGM):
Options to run the simulation with the correct scenarios:

  • With two tracers:

./bin/loveclim-new-run -l PI-bathy -n 10 -r 10 -k -z -I scenario/deglaciation_pmip4_P_T/inputdata_peltier -F scenario/deglaciation_pmip4_P_T/sources-2tr -P scenario/deglaciation_pmip4_P_T/parameters-2tr -s 97801 -S /home/acclimate/nbouttes/iloveclim_degla/data/bathy_P_21000yr_2_CC_FWF_17tr2_ecbilt_clio/ic097801 -v 1

  • Or with 17 tracers (Carbon cycle CC):

./bin/loveclim-new-run -l PI-CC-bathy -n 10 -r 10 -k -z -I scenario/deglaciation_pmip4_P_T/inputdata_peltier -F scenario/deglaciation_pmip4_P_T/sources-17tr -P scenario/deglaciation_pmip4_P_T/parameters-17tr -s 97801 -S /home/acclimate/nbouttes/iloveclim_degla/data/bathy_P_21000yr_2_CC_FWF_17tr2_ecbilt_clio/ic097801 -v 1


Restart from PI: -s 92801 -S /home/acclimate/flhardy/iloveclim/data/PI_20tr_t1.1_0.997_1.15_1.05_1.027_r25_ecbilt_clio/ic092801


Note :
specify correct update_time_fism in input_subgrid2L.f90 (500 for Peltier, 100 for Tarasov)


Note 2: for salinity

  • If no FWF from ice sheets: the global salt mass is conserverd when bathymetry is changed, which modifies the global mean salinity
  • If FWF from ice sheet: the global mean salinity is changed by the fresh water flux from ice sheets, while the global mean salinity is conserved when the bathymetry is changed.


2.1. SO