!----------------------------------------------------------------------- ! Emissions and Stratospheric/Surface Boundary conditions for TM5-Chem !----------------------------------------------------------------------- ! ! Data are expected in two type of locations: ! ! (1) below ${inputdir} (set in your main rc file) for the standard input ! files (land-sea mask, etc...). DO NOT CHANGE THESE. ! ! (2) or in their own ${input.emis.dir.*} (e.g., input.emis.dir.AR5). You ! should change these to match your inventories location. Note that in ! the current template all the inventories location are below the top ! dir ${topdir.dynamic}. This is just a convenience, not mandatory. ! !----------------------------------------------------------------------- ! ! *** MAKE A COPY of this file and include its path into your main rc ! file. Set the flags according to your experiment (T/F keys, AR5 scenario, ! emission year...) and the location of your emissions inventories. ! ----------------------------------------------------------------------- ! convenient top dir for large inventories (EDGAR, AR5, GFED, ...) topdir.dynamic : path/to/somewhere ! CMIP6 Scenario for 2015 and above (expected: SSP1-1.9, SSP1-2.6, ! SSP1-2.6-Ext, SSP2-4.5, SSP3-7.0, SSP3-LowNTCF, SSP5-8.5, ! SSP5-8.5-Ext). Tier 2 scenarios not available. input.CMIP6.SSP : SSP3-7.0 !------------------------ ! Photolysis !------------------------ ! data dir with photolysis specific data input.photo : ${inputdir}/photolysis ! aerosols feedback on photolysis (m7) optics.lookuptable : ${inputdir}/photolysis/lookup_table.nc optics.refractive_indices : ${inputdir}/photolysis/refractive_indices_hdfstyle.nc !------------------------ ! STRATOSPHERE : O3, O3S, CH4, CO and HNO3 are relaxed to climatology dataset !------------------------ ! ! ** For O3: ! CMIP6 data set if input.conc.o3.cmip6=T. ! MSR2 = Multi Sensor Reanalysis, version 2, if input.climat.MSR=T. ! Choose one or the other. ! If neither is selected, ${input.climat.o3vmr} must be ! set to a user input file name (see source code for expected dimension and ! units). However no nudging is performed if the 'without_o3_nudging' cpp ! macro is used. ! ! See: www.temis.nl; Allaart, van der A, manuscript in preparation, 2009) ! ! When CMIP6 is selected, the pre-industrial climatology is used ! if input.conc.o3.cmip6.piclim=T. ! ! ** For CH4 we use HALOE CH4 Climatology (October 1991 to August 2002) if ! input.climat.HALOE=T. Else no nudging is performed. ! ! See technical note: A stratospheric climatology for O3, H2O, CH4, NOx, ! HCl and HF derived from HALOE measurements by J.-U. Grooss and ! J. M. Russell III Atmospheric Chemistry and Physics, 5, 2797-2807, 2005 ! SRef-ID: 1680-7324/acp/2005-5-2797 ! ! If input.conc.ch4.cmip6=T, the HALOE climatology is scaled ! based on the CMIP6 time series of the global and annual mean mixing ratio ! at the surface. ! ! ** HNO3 is prescribed using HNO3:03 ratios from ODIN, if ! input.climat.ODIN=T, or from UARS else. ! ! ** CO is prescribed using CO:03 ratios from ODIN, only if ! input.climat.ODIN=T (no fallback). ! ! ** O3DU (also from MSR) is optionally used in photolysis only. ! ! [See boundary.F90] ! input.conc.o3.cmip6 : F input.conc.o3.cmip6.dir : ${inputdir}/boundary/CMIP6/O3/ input.conc.o3.cmip6.piclim : F ! ! Use Multi Sensor Reanalysis for O3? input.climat.MSR : T input.climat.o3vmr : ${inputdir}/boundary/O3_top/MSR_O3_VMR_HDF/ ! Use O3du (for photolysis)? input.climat.use_o3du : F ! Directory of O3du ? input.climat.o3du : ${inputdir}/boundary/O3_top/MSR_O3_VMR_HDF/ ! Use HALOE for CH4? input.climat.HALOE : T ! Directory of HALOE ? input.climat.ch4vmr : ${inputdir}/boundary/CH4_top/ ! Use ODIN for HNO3 and CO? input.climat.ODIN : T ! Directory for ODIN? input.climat.covmr : ${inputdir}/boundary/ODIN/ ! in case of fallback HNO3:O3 ratio are expected as: ${inputdir}/boundary/HNO3_top/uars_ratio.hdf (hardwired in the code) !------------------------ ! Dry deposition (hardwired) !------------------------ ! files "lsmlai.hdf" and "soilph.hdf" are expected in: ${inputdir}/land !------------------------ ! Set emissions base year (default to simulation year if commented) !------------------------ !input.emis.year : ! !-------------------------------------------------------------------- ! Additional switches to fix the emissions of ! anthropogenic and biomass burning emissions to a specific year ! (as required in AerChemMIP). ! ! The year of emissions can be controlled for the whole group of NTCFs, ! for the sub-groups of aerosol and ozone precursors, ! and/or for the individual species. ! ! Note that settings for individual species or else the subgroup ! to which they belong are leading. ! If these are commented, input.emis.year.ntcf or ! else input.emis.year is used. ! If these are also commented, ! the actual year of simulation is used. ! ! Near-Term Climate Forcers (NTCFs), excl. CH4 !input.emis.year.ntcf : ! ! Aerosol precursors (BC, OC, NH3, SOx) !input.emis.year.aer : !input.emis.year.bc : !input.emis.year.oc : !input.emis.year.sox : !input.emis.year.nh3 : ! ! Ozone precursors (NOx, CO, NMVOCs incl. isoprene and mononterpenes) ! Note that in AerChemMIP, the year for CO should be that for NMVOCs. !input.emis.year.o3 : !input.emis.year.nox : !input.emis.year.co : !input.emis.year.nmvoc : !---------------------------------------------------------------------------- ! Option to fix CMIP6 or MSR O3 mixing ratios to fixed year: ! Note that, for CMIP6, this option applied to the year 1850, ! is not the same as selecting the pre-industrial climatology ! with input.conc.o3.cmip6.piclim=T. input.o3.fixyear : F input.o3.year : ! Option to fix CMIP6 methane boundary conditions and emissions to fixed year input.ch4.fixyear : F input.ch4.year : ! Option to fix CMIP6 CO2 mixing ratio to fixed year: input.co2.fixyear : F input.co2.year : ! Option to prescribe CO2 for the 1pctCO2 or abrupt-4xCO2 DECK simulation ! Only one can be set to True and when this is the case, ! the values of input.co2.fixyear and input.co2.year ! as specified above are not used. ! ! Option to prescribe CO2 as in 1pctCO2: input.co2.1pct: F ! ! Option to prescribe CO2 as in abrupt-4xCO2: input.co2.abrupt-4x: F !------------------------------------------------ ! Set base year for natural emissions ! that don't cover the full period 1850-2100. ! Use 2000 in climate integrations (CMIP6). ! Used for CH4 emissions from LPJ, ! as well as for MACC & MEGAN. !------------------------------------------------ input.natemis.year : 2000 ! ---------------------------------------- ! Anthropogenic emis (choose ONE: CMIP6 (1850-2100) or AR5(1850-2100) or EDGAR4(1970-2005/8) or MACCITY(1960-2020) ) ! ---------------------------------------- use_cmip6 : F input.emis.dir.CMIP6 : ${topdir.dynamic}/CMIP6 use_ar5 : F input.emis.dir.AR5 : ${topdir.dynamic}/AR5 ! AR5 scenario: choose b/w RCP26, RCP45, RCP60, RCP85 and 'hist' for historical input.emis.AR5.RCP : RCP45 use_edgar4 : F input.emis.dir.ED41 : ${topdir.dynamic}/EDGAR4 use_maccity : F ! dir for MACC-city is "input.emis.dir.MACC". [same data + IPCC aircraft emiss] !***** it is important that the path to AR5 and EDGAR are correct even if the ***** !***** use_ar5 and use_edgar4 are set to F. Because maccity is missing CH4 and ***** !***** reverts to EDGAR for CH4, and because (if using M7) AR5 is always used ***** !***** to get BC and OC emissions. ***** ! ---------------------------------------- ! Biomass burning (choose one: CMIP6BMB (1850-2100), GFED3 (1997-2010), RETRO_FIRES(1960-2000) or AR5_FIRES) ! ---------------------------------------- use_cmip6_fires : F use_ar5_fires : F use_retro_fires : F use_gfed3 : F input.emis.dir.gfed : ${topdir.dynamic}/GFED3 input.emis.dir.retro : ${topdir.dynamic}/RETRO ! apply daily cycle to BMB in the tropics ! (based on isoprene and not applied to BC/POM) input.emis.bb.dailycycle : F ! ---------------------------------------- ! Natural emissions ! ---------------------------------------- ! all gases : MACC use_macc : T input.emis.dir.MACC : ${topdir.dynamic}/MACCity ! use MEGAN v1 (1980-2010) for biogenic sources ! (will replaces 'bio' src from MACC for ISOP, CO, and NMVOC) use_megan : T input.emis.dir.MEGAN : ${topdir.dynamic}/MEGAN ! CH4 : add HYMN/LPJ (see readme-hymn) use_lpj : T use_hymn : T input.emis.dir.natch4 : ${inputdir}/natural_emissions/reactive_gases/CH4/HYMN ! RN 222 (file: RN222_WMO2004.hdf) input.emis.dir.rn222 : ${inputdir}/natural_emissions/tracer ! DMS (files: "DMSland.hdf" and "DMSconc.hdf") input.emis.dir.dms : ${inputdir}/natural_emissions/reactive_gases/DMS ! ---------------------------------------- ! Aerosols ! ---------------------------------------- ! DUST : choose between AEROCOM (monthly, fix year:2000), TEGEN-VIGNATI ! (monthly, location unknown=> option unavailable until further notice), ! and ONLINE input.emis.dust : ONLINE ! directory for that choice input.emis.dir.dust : ${inputdir}/aerosols/Dust/${input.emis.dust} ! POM : directory for anthropogenic SOA file (SOA.hdf) input.emis.dir.aerocom : ${inputdir}/aerosols/SOA ! New particle formation scheme ! 1 Vehkamaki et al. 2002 (so4) ! 2 Kulmala et al. 1996 (so4) ! 3 Paasonen et al. 2010 (organic+so4) + Vehkamaki et al. ! 4 Riccobono et al. 2014 + Vehkamaki et al. input.nucleation.scheme : 4 !SOA scheme !0 POM AeroCom (aitkenmodes) !1 POM distribution according to volatility (5 modes) (not implemented) !2 monoterpene+isoprene oxidation + condensation input.soa.scheme : 2 !Use also isoprene yields for ELVOC and SVOC production !Default value True input.soa.isoprene_on : T !Size of formed particles in KK parameterisation in nm (default: 5.0) input.KK.d_form : 5.0 ! ---------------------------------------- ! NOx extra sources ! ---------------------------------------- ! MODIS input.onlinenox.dir : ${inputdir}/input/glb1x1 ! Lightning NOx uses Land fraction, expected as: ${inputdir}/land/landfraction.hdf (hardwired) ! ---------------------------------------- ! Nudging CH4 [see emission_CH4.F90] ! ---------------------------------------- ! If input.conc.ch4.cmip6 is set to T: ! - CMIP6 zonal mean surface mixing ratios used in the lower troposphere ! - HALOE climatology of stratospheric CH4 mixing ratios scaled ! based on CMIP6 time series of global annual mean mixing ratio at surface ! (input.climat.HALOE forced to T) input.conc.ch4.cmip6 : F input.conc.ch4.cmip6.dir : ${inputdir}/boundary/CMIP6/CH4/ ! Alternatively, if input.emis.ch4.single is set to T, a single mixing ratio ! (input.emis.ch4.fixed_ppb) is prescribed at the surface, or [TODO: ! doublecheck is true] in the whole atmosphere (with HALOE climatology ! switched off): input.emis.ch4.single : F input.emis.ch4.fixed_ppb : 1760.0 input.emis.ch4.fix3d : F ! Else read the zonal background field from NOAA/GMD mean surface fields in ! input.emis.ch4.surf for year/month (without scaling of the HALOE ! climatology). ! ! This zonal mean field is used for nudging CH4 emissions: ! - up to 550 hPa, if with_ch4_emission is used [RECOMMENDED] ! - in the two lowest layers if with_ch4_emission is NOT used, and input.emis.ch4.fix3d is F ! - in all layers if with_ch4_emission is NOT used, and input.emis.ch4.fix3d is T ! input.emis.ch4.surf : ${inputdir}/boundary/CH4_surf/ ! ---------------------------------------- ! CO2 mixing ratio used in pH calculation for aqueous chemistry ! ---------------------------------------- ! If input.conc.co2.cmip6 is set to T (RECOMMENDED), ! global annual mean mixing ratios from CMIP6 are used; ! otherwise, it is fixed to a value for the year 2000. input.conc.co2.cmip6 : T input.conc.co2.cmip6.dir : ${inputdir}/boundary/CMIP6/CO2/ !------------------------ ! Cariolle !------------------------ ! Does not applied