Version 1.4 by Peter van Velthoven: various additions based on input by the ocean biogeochemists.
Previous versions:
Version 1.3 by Peter van Velthoven: modifications based on further discussions
with Jonathan Gregory .
Version 1.2, 25 May 2003, modifications based on comments by Jonathan Gregory
Version 1.1, 28 february 2002, first draft
Only the standard_names co2, so4 and o3 are
currently defined in the CF
standard name guidelines. All others need to be proposed to the CF group.
For consistency with all the others co2, so4 and o3
should be made obsolete (provide aliases for the few that use them). They should
be replaced by carbon_dioxide, sulfate_aerosol and ozone.
For water vapor there is no standard_name h2o, but the standard_name specific_humidity
(kg/kg) has been defined in the hydrology
table. Note that this is a mass_fraction or mass mixing ratio. Species
quantities should preferably be archived as volume mixing ratios (mole_fraction)
with canonical unit dimensionless (parts per volume). Aerosols are an exception;
mass_concentration (with canonical unit kg m-3) seems more suitable
for aerosols.
All standard names should be in English spelt the American way.
The atmospheric chemical species are all in one of the following categories:
| CF standard_name | Species | Chemical formula |
| carbon_dioxide alias:co2 | Carbon dioxide * | CO2 |
| ozone alias: o3 | Ozone **, *** | O3 |
| nitrogen_oxide | Nitrogen oxide | NO |
| hydrogen_peroxide | Hydrogen peroxide | H2O2 |
| methane | Methane | CH4 |
| carbon_monoxide | Carbon monoxide | CO |
| nitric_acid | Nitric acid | HNO3 |
| methyl_hydrogen_peroxide | Methyl hydrogen peroxide | CH3O2H |
| formaldehyde | Formaldehyde | CH2O |
| peroxy_acetyl_nitrate | Peroxy acetyl nitrate (PAN) | CH3C(O)O2NO2 |
| sulfur_dioxide | Sulfur dioxide | SO2 |
| dimethyl_sulfide | Dimethyl sulfide (DMS) *** | CH3SCH3 |
| ammonia | Ammonia | NH3 |
| ammonium | Ammonium | NH4 |
| methane_sulfonic_acid | Methane sulfonic acid (MSA) | CH3SO2OH |
| hydroperoxy_radical | Hydroperoxy radical | HO2 |
| methyl_peroxy_radical | Methyl peroxy radical | CH3O2 |
| hydroxyl_radical | Hydroxyl radical (hydroxy radical) | OH |
| nitrogen_dioxide | Nitrogen dioxide | NO2 |
| nitrate_radical | Nitrate radical | NO3 |
| dinitrogen_pentoxide | Dinitrogen pentoxide | N2O5 |
| _nitric_acid | Nitric acid | HNO3 |
| peroxy_nitric_acid | Peroxy nitric acid | HNO4 |
| peroxy_acetyl_radical | Peroxy acetyl radical | C2O3 |
| oxygen_radical_in_1D_state | Oxygen radical in the 1D (excited) state | O(1-D) |
| ethane | ethane | C2H6 |
| ethylene | ethylene or ethene | C2H4 |
| acetylene | acetylene | C2H2 |
| propane | propane | C3H8 |
| propene | propene | C3H6 |
| acetone | acetone | C3H6O |
| butane | butane | C4H10 |
| methyl_glyoxal | Methyl glyoxal | CH3C(O)C(O)H |
| isoprene | Isoprene, 2-methyl-1,3-butadiene | C5H8 |
| Additional ocean species: | ||
|---|---|---|
| phosphorus | Phosphorus | P |
| phosphate | Phosphate | PO4 |
| organic_phosphate | Organic phosphate | PO4 with C? |
| silicon | Silicon | Si |
| silicate | Silicate | SiO3 |
| silicic_acid | Silicate | SiO3 |
| iron | Iron | Fe |
| oxygen | Oxygen (atomic) | O |
| oxygen_18 | Oxygen 18 | 18O |
| molecular_oxygen | Molecular oxygen | O2 |
| nitrogen | Nitrogen | N |
| nitrate | Nitrate | NO3-? |
| carbon | Carbon | C |
| inorganic_carbon | Inorganic carbon | C |
| organic_carbon | Organic carbon | C |
| carbonate | Carbonate | CO3- |
| carbon_13 | Carbon 13 | 13C |
| carbon_14 | Carbon 14 | 14C |
| hydrogen | Hydrogen (atomic) | H |
| calcite | Calcite | Ca? |
* already defined in CF
** for ozone mass_fraction_of_o3_in_air and mole_fraction_of_o3_in_air have already been defined. The first is a mass mixing ratio, the second a volume mixing ratio. The atmospheric chemists prefer mass_fraction_of_ozone_in_air and mole_fraction_of_ozone_in_air as standard_names. See the list of constructs below.
*** used both in the atmosphere and the ocean (O3, DMS)
In some chemical schemes, such as CBM IV, chemical species are lumped, i.e.
a certain reaction rate is associated with a certain group of species showing
similar chemical behaviour. In lumping, correctors may need to be added to get
the correct chemical behaviour. The following standard_names will be used for
lumped species:
| CF standard name | Lumped species (from the modified CBMIV-chemistry in TM) | Chemical formula |
| paraffinic_carbon_bonds | Paraffinic carbon bonds | C-C |
| olefinic_carbon_bonds | Olefinic carbon bonds | |
| aldehydes_higher_than_2 | aldehydes with more than one C atom, Acetaldehyde (=ethanal) and higher aldehydes | RCH=O (excluding the case R equals H: CH2=O, formaldehyde) |
| organic_peroxides | lumped higher organic peroxides | ROOH |
| organic_nitrates | lumped alkyl nitrates, organic nitrates | RNO3 |
| secondary_organic_oxy_radical | Secondary organic oxy radical | ROR |
| alkyl_peroxy_radicals | alkyl peroxy radicals | XO2 |
| intermediate_product_of_isoprene_oxidation | intermediate product of isoprene oxidation | XO2N |
Here R is CH3+C2H5+... and X is CH3N+C2H5N+.. If _higher_than_2_
is included in the name, CH3 resp. CH3N are not included in the sum of compounds.
Perhaps a prefix such as cb4_ should be used to identify the
lumping scheme.
The following standard_names refer to families of species:
| CF standard_name | Family |
| nox | NO and NO2 |
| noy | reactive nitrogen compounds (excludes n2o) |
| hox | OH and HO2 |
The following standard_names refer to aerosol species:
| CF standard_name | Aerosol species | Chemical formula |
| so4 should become an alias for sulfate_aerosol | sulfate aerosol | H2SO4 |
| nitrate_aerosol | nitrate aerosol | HNO3 |
| ammonium_sulfate_aerosol | ammonium sulfate aerosol | NH4SO4 |
| sea_salt_aerosol | sea salt aerosol | NaCl |
| organic_aerosol_from_terpenes ? | Secondary aeresol formed from terpenes ? (check with MPI) | |
| organic_carbon_aerosol | organic carbon aerosol | |
| hydrophobic_organic_carbon_aerosol | hydrophobic organic carbon aerosol | |
| hydrophylic_organic_carbon_aerosol | hydrophylic organic carbon aerosol | |
| black_carbon_aerosol | black carbon aerosol | |
| hydrophylic_black_carbon_aerosol | hydrophylic black carbon aerosol | |
| hydrophobic_black_carbon_aerosol | hydrophobic black carbon aerosol | |
| dust_aerosol | dust aerosol |
| CF standard_name | Biological acronym |
| phytoplankton | |
| nanophytoplankton | |
| microzooplankton | |
| zooplankton | |
| mesozooplankton | |
| diatoms | |
| coccolithophorid | cocco |
| sediment | |
| detritus | POC, calcium, opal |
| chlorophyll | Clf |
I propose the following guidelines for the construction of further standard_names of atmospheric chemistry parameters:
| Construct | Canonical unit |
|---|---|
| mole_fraction_of_.._in_air | 1 (dimensionless, ppv) |
| as alias we may wish to define also | |
| volume_mixing_ratio_of_.._in_air | 1 (dimensionless, ppv) |
| mass_fraction_of_.._in_air | 1 (dimensionless, kg/kg) |
| partial_pressure_of_.._in_air | Pa |
| mass_concentration_of_.._in_air | kg m-3 |
| number_concentration_of_.._in_air | m-3 (molecules or particles per m3) |
| mole_concentration_of_.._in_air | mole m-3 (moles per m3) |
| dry_deposition_flux_of_.. | mole m-2s-1 * |
| wet_deposition_flux_of_.. | mole m-2s-1* |
| surface_emission_of_.. | mole m-2s-1 * |
| volume_emission_of_.._in_air | mole m-3s-1 * |
| chemical_production_of_.._in_air_due_to_..** | s-1 (ppv/hr) |
| chemical_loss_of_..in_air_due_to_..** | s-1 (ppv/hr) |
| gross_chemical_production_of_.._in_air | s-1 (ppv/hr) |
| chemical_loss_of_..in_air | s-1 (ppv/hr) |
| net_chemical_production_of_.._in air | s-1 (ppv/hr) |
| tendency_of_mole_fraction_of_.._in_air_due_to_*** | s-1 (ppv/hr) |
| atmosphere_mole_content_of_.. **** | mole m-2 (or Dobson Units, 1 DU = 2.69 x 1e20 molecules/m2) |
* if fluxes would be expressed in kg/(m2s), one would have to know the atomic mass of the particular species for conversion to mass. In practice not always the same number is used for this. E.g. for NOx the mass of N and of NO2 are both sometimes used. Hence molecules/(m2s) or moles/(m2s) would seem preferable.
**reaction_of_.._with_.., photolysis, photolysis_of_..*** advection, diffusion, convection, scavenging, evaporation, emission (the last is used for volume emissions such as from aircraft and lightning)
**** atmosphere_mole_content_of_.. has units mole m-2. Note that many other content variables have unit kg/m2 (as for so4, sulfate aerosol); see also *.
In order to describe size ranges of aerosols an extra dimension should be used.
In order to describe in-cloud processes the standard-names may need to be catenated with cloudy:
| Construct |
| in_cloudy_air |
In order to describe tracers originating from a certain atmospheric compartment use the following construct:
| Standard name | Example | Variable |
| mole_fraction_of_compartment_.. | mole_fraction_of_stratospheric_ozone | stratospheric ozone tracer, ozone from the stratosphere |
The following are guidelines for the construction of further standard names of oceanic chemistry and biological parameters:
| Construct | Canonical unit |
|---|---|
| mole_concentration_of_.._in_sea_water | mole m-3 |
| ocean_mole_content_of_.. | mole m-2 |
| surface_mole_concentration_of_.._in_sea_water | mole m-3 |
| mole_concentration_of_.._dissolved_in_sea_water | mole m-3 |
| mole_concentration_of_particulate_.._in_sea_water | mole m-3 |
| mole_concentration_of_.._in_ocean_sediment_pores | mole m-3 |
| surface_mole_concentration_of_.._in_diatoms_in_sea_water
surface_mole_concentration_of_.._in_coccolithorid_in_sea_water surface_mole_concentration_of_.._in_nanophytoplankton_in_sea_water | mole m-3 |
| tendency_of_mole_concentration_of_.._in_sea_water_due_to.. | mole m-3 s-1 |
| Standard name | Meaning | Canonical unit |
|---|---|---|
| alkalinity | mu eq / L | |
| acidity | acidity, Ph |