Changes between Version 13 and Version 14 of Documentation/UserGuide/FutureTime
- Timestamp:
- 2016-11-26T21:48:10+01:00 (7 years ago)
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Documentation/UserGuide/FutureTime
v13 v14 63 63 Keep the default setting for solaire (1366.0896 Wm-2). Change the settings for co2_pmm = 0.5384E+03, ch4_ppb = 0.1576E+04, N2O_ppb = 0.372E+03, CFC11_ppt = 3.2E+01, CFC12_ppt = 0.185E+03. 64 64 65 Now the ELI-128x118x39-2 010 can be launched. It takes about 70 seconds per year so in this example it will take over 30 minutes to complete this 30-year job66 {{{ 67 ccc_msub Job_ELI-128x118x39-2 010-RCP4565 Now the ELI-128x118x39-2100 can be launched. It takes about 70 seconds per year so in this example it will take over 30 minutes to complete this 30-year job 66 {{{ 67 ccc_msub Job_ELI-128x118x39-2100-RCP45 68 68 }}} 69 69 … … 220 220 221 221 222 === PARAM/config.def_ future===222 === PARAM/config.def_rcp45 === 223 223 Go to the PARAM folder and rename config.def_actuel. 224 224 {{{ … … 234 234 }}} 235 235 All other settings are set to _AUTO_ and should thus be automatically taken into account. 236 237 238 [[BR]]239 [[BR]]240 [[BR]]241 [[BR]]242 243 +++ CONTINUE, CHECK, ADJUST & TEST +++244 245 [[BR]]246 [[BR]]247 236 248 237 === COMP/lmdz.card === … … 251 240 LMDZ_Physics=NPv3.1 252 241 }}} 253 For the old physics set in COMP/lmdz.card242 For the old physics (that is what we use here) set in COMP/lmdz.card 254 243 {{{ 255 244 LMDZ_Physics=AP 256 245 }}} 257 246 258 The aerosols that are being used are set in PARAM/config.def_preind (see above). In COMP/lmdz.card we have some additional manual control but it is better not to touch it. 247 Adjust the name of the BC files to your ELI jobname 248 {{{ 249 CREATE=ELI-${RESOL_ATM_3D}-2100 250 }}} 251 252 Use the desired config file 253 {{{ 254 ConfType=rcp45 255 }}} 256 257 258 The aerosols that are being used are set in PARAM/config.def_rcp45 (see above). In COMP/lmdz.card we have some additional manual control but it is better not to touch it. 259 259 {{{ 260 260 #flag_aerosol=6 … … 281 281 }}} 282 282 283 The aerosols have to be interpolated to the zoomed model grid. The years 1980-2000 for HISTORIQUE run version _v5 have been done. They are found at the standard place : /ccc/work/cont003/dsm/p86ipsl/IGCM/BC/ATM/LMDZ/LMD128118/AR5/HISTORIQUE . You need to change _v3 into _v5 in lmdz.card to use these files. Similar to the pre-industrial run in which we only used the aerosols of 1860 we will now only use the aerosols of 2000 to avoid adding more variability to the present day runs compared to the pre-industrial run. Because we want to calculate the net climate effect of both biogeochemical and biophysical effects of forest manangement and land cover change, we have to recalculate the atmospheric CO2 concentration for the different treatments. To do so we first applied the BERN2.5 box model to account for the equilibrium between the atmosphere, the land and the oceans (thus the reason why ~40% of the emissions stay in the atmosphere). Following we converted this CO2 uptake/release into a change in atmospheric CO2 concentration. Finally, this change was subtracted from the present day atmospheric CO2. Note that $$$ below should be BC, BCF, BCL or BCLF depending on the experimental treatment.283 The aerosols have to be interpolated to the zoomed model grid. The years 1980-2000 for HISTORIQUE run version _v5 have been done. They are found at the standard place : /ccc/work/cont003/dsm/p86ipsl/IGCM/BC/ATM/LMDZ/LMD128118/AR5/HISTORIQUE . You need to change _v3 into _v5 in lmdz.card to use these files. Similar to the pre-industrial run in which we only used the aerosols of 1860 we will now only use the aerosols of 2000 to avoid adding more variability to the present day runs compared to the pre-industrial run. Because we want to calculate the net climate effect of both biogeochemical and biophysical effects of forest manangement and land cover change, we have to recalculate the atmospheric CO2 concentration for the different treatments. To do so we first applied the BERN2.5 box model to account for the equilibrium between the atmosphere, the land and the oceans (thus the reason why ~40% of the emissions stay in the atmosphere). Following we converted this CO2 uptake/release into a change in atmospheric CO2 concentration. Finally, this change was subtracted from the present day atmospheric CO2. Note that $$$ below should be name of the optimised scenario depending on the experiment. 284 284 {{{ 285 285 [InitialStateFiles] … … 294 294 # With AR5 ozone(tropo + strato from LMDZOR-INCA-REPROBUS simulations) 295 295 ListNonDel= (/ccc/work/cont003/dofoco/dofoco/INPUT_FILES/ATM_COMP/SOLAR_ACTUAL.txt, SOLARANDVOLCANOES.txt),\ 296 (/ccc/work/cont003/dofoco/dofoco/INPUT_FILES/ATM_COMP/CO2_ ACTUAL_$$$.txt, CO2.txt),\297 (/ccc/work/cont003/dofoco/dofoco/INPUT_FILES/ATM_COMP/CH4_ ACTUAL.txt, CH4.txt),\298 (/ccc/work/cont003/dofoco/dofoco/INPUT_FILES/ATM_COMP/N2O_ ACTUAL.txt, N2O.txt),\299 (/ccc/work/cont003/dofoco/dofoco/INPUT_FILES/ATM_COMP/CFC11_ ACTUAL.txt, CFC11.txt),\300 (/ccc/work/cont003/dofoco/dofoco/INPUT_FILES/ATM_COMP/CFC12_ ACTUAL.txt, CFC12.txt),\296 (/ccc/work/cont003/dofoco/dofoco/INPUT_FILES/ATM_COMP/CO2_RCP45_$$$.txt, CO2.txt),\ 297 (/ccc/work/cont003/dofoco/dofoco/INPUT_FILES/ATM_COMP/CH4_RCP45.txt, CH4.txt),\ 298 (/ccc/work/cont003/dofoco/dofoco/INPUT_FILES/ATM_COMP/N2O_RCP45.txt, N2O.txt),\ 299 (/ccc/work/cont003/dofoco/dofoco/INPUT_FILES/ATM_COMP/CFC11_RCP45.txt, CFC11.txt),\ 300 (/ccc/work/cont003/dofoco/dofoco/INPUT_FILES/ATM_COMP/CFC12_RCP45.txt, CFC12.txt),\ 301 301 (${R_BC}/ATM/${config_UserChoices_TagName}/${RESOL_ATM}/AR5/HISTORIQUE/aerosols_11YearsClim_1860_v5.nc, aerosols.nat.nc) 302 302 … … 309 309 (${ARCHIVE}/IGCM_OUT/LMDZ/${CREATE}/ATM/Output/Boundary/${CREATE}_${year}_climoz_LMDZ.nc, climoz_LMDZ.nc, 1:12:) 310 310 311 }}} 312 313 Pre-defined present day settings (TOA solar incoming radiation, atmospheric CO2, CH4 and N2O and aerosols (see above)) should be set by changing 314 {{{ 315 ConfType=actuel 316 }}} 317 318 Alternatively this setting can be hard coded by changing ${ConfType} into preind in the following line. The first option seems more direct. 319 {{{ 320 (${SUBMIT_DIR}/PARAM/config.def_actual, config.def), \ 321 }}} 322 323 Beacuse we have set the radiation and atmospheric concentrations to _AUTO_ in PARAM/config.def_actual it looks like the model then uses the boundary files specified in COMP/lmdz.card 311 312 Hard code ${ConfType} in the following line 313 {{{ 314 (${SUBMIT_DIR}/PARAM/config.def_rcp45, config.def), \ 315 }}} 316 317 Beacuse we have set the radiation and atmospheric concentrations to _AUTO_ in PARAM/config.def_rcp45 it looks like the model then uses the boundary files specified in COMP/lmdz.card 324 318 325 319 … … 333 327 guide_P= n 334 328 guide_Q= n 335 tau_min_u=0.0 5336 tau_max_u= 10.337 tau_min_v=0.0 5338 tau_max_v= 10.339 }}} 340 This means that outside the zoom, the wind is nudged every 86400*0.0 5 seconds (about 1h12min), which is considered fairly strong but necessary for an intense zoom. Inside the zoom, the winds are slightly nudged every 10 days.329 tau_min_u=0.0208333 330 tau_max_u=0.125 331 tau_min_v=0.0208333 332 tau_max_v=0.125 333 }}} 334 This means that outside the zoom, the wind is nudged every 86400*0.0208 seconds (about 30min), which is considered fairly strong but necessary for an intense zoom. Inside the zoom, the winds are slightly nudged every 10 days. 341 335 342 336 === PARAM/physiq.def_L39_NPv3.1 ===