GEOS–Chem v9–01–03 Online User's Guide
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Appendix 1: GEOS–Chem Tracers, by Simulation
With GEOS–Chem, you can perform several different types of chemistry simulations. For each simulation, we provide a list of advected tracers below.
A1.1 NOx–Ox–hydrocarbon–aerosol simulations
Advected tracers fall into two categories:
Many advected tracers are also listed as individual species in the chemical mechanism. Please consult Appendix 6 for a complete list of chemical species in GEOS–Chem.
We specify several hydrocarbon tracers (those listed in BOLD ITALICS) as atoms C instead of molecules tracer. We assign to these a molecular weight of 12 g/mole. The number of moles C per moles tracer is listed below.
You can select from different chemistry mechanism options for the NOx–Ox–hydrocarbon–aerosol simulations. In the following table we give the tracers for each option: the standard mechanism, the SOA mechanism, the dicarbonyls mechanism and the Caltech isoprene mechanism.
For more information, please see:
# | Name | Description | g/mole | mole C/ mole tracer |
---|---|---|---|---|
Standard
mechanism |
||||
1 | NOx | NO + NO2+ NO3 + HNO2 | 46 | - |
2 | Ox | O3 + NO2 + 2NO3 | 48 | - |
3 | PAN | Peroxyacetyl Nitrate | 121 | - |
4 | CO | Carbon Monoxide | 28 | - |
5 | ALK4 | Lumped >= C4 Alkanes | 12 | 4 |
6 | ISOP | Isoprene | 12 | 5 |
7 | HNO3 | Nitric Acid | 63 | - |
8 | H2O2 | Hydrogen Peroxide | 34 | - |
9 | ACET | Acetone | 12 | 3 |
10 | MEK | Methyl Ethyl Ketone | 12 | 4 |
11 | ALD2 | Acetaldehyde | 12 | 2 |
12 | RCHO | Lumped Aldehyde >= C3 | 58 | - |
13 | MVK | Methyl Vinyl Ketone | 70 | - |
14 | MACR | Methacrolein | 70 | - |
15 | PMN | Peroxymethacroyl Nitrate | 147 | - |
16 | PPN | Lumped Peroxypropionyl Nitrate | 135 | - |
17 | R4N2 | Lumped Alkyl Nitrate | 119 | - |
18 | PRPE | Lumped >= C3 Alkenes | 12 | 3 |
19 | C3H8 | Propane | 12 | 3 |
20 | CH2O | Formaldehyde | 30 | - |
21 | C2H6 | Ethane | 12 | 2 |
22 | N2O5 | Dinitrogen Pentoxide | 105 | - |
23 | HNO4 | Pernitric Acid | 79 | - |
24 | MP | Methyl Hydro Peroxide | 48 | - |
25 | DMS | Dimethyl Sulfide | 62 | - |
26 | SO2 | Sulfur Dioxide | 64 | - |
27 | SO4 | Sulfate | 96 | - |
28 | SO4s | Sulfate on surface of sea-salt aerosol | 96 | - |
29 | MSA | Methyl Sulfonic Acid | 96 | - |
30 | NH3 | Ammonia | 17 | - |
31 | NH4 | Ammonium | 18 | - |
32 | NIT | Inorganic nitrates | 62 | - |
33 | NITs | Inorganic nitrates on surface of sea-salt aerosol | 62 | - |
34 | BCPI | Hydrophilic black carbon aerosol | 12 | 1 |
35 | OCPI | Hydrophilic organic carbon aerosol | 12 | 1 |
36 | BCPO | Hydrophobic black carbon aerosol | 12 | 1 |
37 | OCPO | Hydrophobic organic carbon aerosol | 12 | 1 |
38 | DST1 | Dust aerosol, Reff = 0.7 microns | 29 | - |
39 | DST2 | Dust aerosol, Reff = 1.4 microns | 29 | - |
40 | DST3 | Dust aerosol, Reff = 2.4 microns | 29 | - |
41 | DST4 | Dust aerosol, Reff = 4.5 microns | 29 | - |
42 | SALA | Accumulation mode sea salt aerosol (Reff = 0.01 – 0.5 microns) |
36 | - |
43 | SALC | Coarse mode sea salt aerosol (Reff = 0.5 – 8 microns) |
36 | - |
44 | Br2 | Molecular bromine | 160 | - |
45 | Br | Bromine radical, or atomic bromine | 80 | - |
46 | BrO | Bromine monoxide | 96 | - |
47 | HOBr | Hypobromous acid | 97 | - |
48 | HBr | Hypobromic acid | 81 | - |
49 | BrNO2 | Nitryl bromide | 126 | - |
50 | BrNO3 | Bromine nitrate | 142 | - |
51 | CHBr3 | Bromoform, or tribromomethane | 253 | - |
52 | CH2Br2 | Dibromomethane | 174 | - |
53 | CH3Br | Methyl bromide | 95 | - |
SOA mechanism | ||||
1-37 | Same tracers as for the standard mechanism | |||
38 | ALPH | A-pinene, B-pinene, sabinene, carene, terpenoid ketones | 136.23 | - |
39 | LIMO | Limonene | 136.23 | - |
40 | ALCO | Myrcene, terpenoid alcohols, ocimene | 142 | - |
41 | SOG1 | Lump of gas products of first 3 (ALPH + LIMO + TERP) hydrocarbon oxidation | 150 | - |
42 | SOG2 | Gas product of ALCO oxidation | 160 | - |
43 | SOG3 | Gas product of SESQ oxidation | 220 | - |
44 | SOG4 | Gas product of ISOP oxidation | 130 | - |
45 | SOG5 | Gas product of aromatics oxidation | 150 | - |
46 | SOA1 | Lump of aerosol products of first 3 (ALPH + LIMO + TERP) hydrocarbon oxidation | 150 | - |
47 | SOA2 | Aerosol product of ALCO oxidation | 160 | - |
48 | SOA3 | Aerosol product of SESQ oxidation | 220 | - |
49 | SOA4 | Aerosol product of ISOP oxidation | 130 | - |
50 | SOA5 | Aerosol product of aromatics oxidation | 150 | - |
51-56 | Insert tracers 38-43 (dusts and sea salts) from standard simulation. | |||
57 | BENZ | Benzene | 12 | 6 |
58 | TOLU | Toluene | 12 | 7 |
59 | XYLE | Xylene | 12 | 8 |
Dicarbonyls mechanism | ||||
1-56 | Same tracers as SOA simulation | |||
57 | GLYX | Glyoxal | 58 | - |
58 | MGLY | Methylglyoxal | 72 | - |
59 | BENZ | Benzene | 12 | 6 |
60 | TOLU | Toluene | 12 | 7 |
61 | XYLE | Xylene | 12 | 8 |
62 | MONX | Monoterpenes | 12 | 10 |
63 | SOAG | SOA product of GLYX | 58 | - |
64 | SOAM | SOA product of MGLY | 72 | - |
65 | C2H4 | Ethene | 12 | 2 |
66 | C2H2 | Acetylene | 12 | 2 |
67 | MBO | 2-methyl-3-bute-2-nol | 12 | 5 |
68 | GLYC | Glycoaldehyde | 60 | - |
69 | HAC | Hydroxyacetone | 74 | - |
70 | ACRPAN | APAN (CH2CHC(O)OONO2) | 133 | - |
71 | ENPAN | ENPAN (NO2OCH2C(O)OONO2) | 182 | - |
72 | GLPAN | Peroxyacylnitrate from GLCO3 | 137 | - |
73 | GPAN | Peroxyacylnitrate from GCO3 | 135 | - |
74 | MPAN | 2-methyl-1-oxo-2-propenyl nitroperoxyde | 132 | - |
75 | NIPAN | NIPAN (NO2OCH2CCH3CHC(O)OONO2, C5PAN18) | 224 | - |
Caltech isoprene mechanism | ||||
1-43 | Same tracers as standard simulation (without bromine species) | |||
44 | HCOOH | Formic acid | 46 | - |
45 | ACTA | Acetic acid | 60 | - |
46 | ISOPN | Isoprene nitrate | 147 | - |
47 | MOBA | 5C acid from isoprene | 114 | - |
48 | PROPNN | Propanone nitrate | 109 | - |
49 | HAC | Hydroxyacetone | 74 | - |
50 | GLYC | Glycolaldehyde | 60 | - |
51 | MMN | Nitrate from MACR + MVK | 149 | - |
52 | RIP | Peroxide from RIO2 | 118 | - |
53 | IEPOX | Isoprene epoxide | 118 | - |
54 | PYPAN | Pyruvic acid PAN | 149 | - |
55 | MAP | Peroxyacetic acid | 76 | - |
56 | AP | 76 | - |
NOTES:
Online 2dy ORG AEROSOLS : F
Online dicarb. chem. : F
A1.2 Offine aersosol simulations
You can run a GEOS–Chem "offline" aerosol simulation without having to call the SMVGEAR II or KPP solver. The tracer list is below.
For more information, please see:
# | Name | Description | g/mole |
---|---|---|---|
1 | DMS | Dimethyl sulfide | 62 |
2 | SO2 | Sulfur dioxide | 64 |
3 | SO4 | Sulfate | 96 |
4 | SO4s | Sulfate on surface of sea salt aerosol | 96 |
5 | MSA | Methane Sulfionic Acid | 96 |
6 | NH3 | Ammonia | 17 |
7 | NH4 | Ammonium | 18 |
8 | NIT | Inorganic sulfur nitrates | 62 |
9 | NITs | Inorganic sulfur nitrates on surface of sea-salt aerosol | 62 |
10 | BCPI | Hydrophilic black carbon aerosol | 12 |
11 | OCPI | Hydrophilic organic carbon aerosol | 12 |
12 | BCPO | Hydrophobic black carbon aerosol | 12 |
13 | OCPO | Hydrophobic organic carbon aerosol | 12 |
14 | ALPH | A-pinene, B-pinene, sabinene, carene, terpenoid ketones | 136.23 |
15 | LIMO | Limonene | 136.23 |
16 | ALCO | Myrcene, terpenoid alcohols, ocimene | 142 |
17 | SOG1 | Lump of gas products of first 3 (ALPH+LIMO+TERP) hydrocarbon oxidation |
150 |
18 | SOG2 | Gas product of ALCO oxidation | 160 |
19 | SOG3 | Gas product of SESQ oxidation | 220 |
20 | SOG4 | Gas product of ISOP oxidation | 130 |
21 | SOG5 | Gas product of aromatics oxidation | 150 |
22 | SOA1 | Lump of aerosol products of first 3 (ALPH+LIMO+TERP) hydrocarbon oxidation |
150 |
23 | SOA2 | Aerosol product of ALCO oxidation | 160 |
24 | SOA3 | Aerosol product of SESQ oxidation | 220 |
25 | SOA4 | Aerosol product of ISOP oxidation | 130 |
26 | SOA5 | Aerosol product of aromatics oxidation | 150 |
27 | DST1 | Dust aerosol, Reff = 0.7 microns | 29 |
28 | DST2 | Dust aerosol, Reff = 1.4 microns | 29 |
29 | DST3 | Dust aerosol, Reff = 2.4 microns | 29 |
30 | DST4 | Dust aerosol, Reff = 4.5 microns | 29 |
31 | SALA | Accumulation mode sea salt aerosol (Reff = 0.1 – 2.5 microns) |
36 |
32 | SALC | Coarse mode sea salt aerosol (Reff = 2.5 – 4 microns) |
36 |
NOTE: You may omit the secondary organic aerosol tracers (ALPH, LIMO, ALCO, SOG1, SOG2, SOG3, SOG4, SOG5, SOA1, SOA2, SOA3, SOA4, SOA5) by setting the following switches in the aerosol menu section of the input.geos file.
Online 2dy ORG AEROSOLS : F
If you omit the secondary organic aerosol tracers then there will be a total of 18 tracers.
A1.3 Total CO2 and Tagged CO2 simulations
Ray Nassar updated the CO2 simulation in GEOS–Chem v8–03–02.
For more information, please see:
# | Name | Description | g/mole |
---|---|---|---|
1 | CO2 | Total CO2 | 44 |
If you wish, you may add tracers for additional CO2 sources: |
|||
2 | CO2ff | CO2 from fossil fuel emissions | 44 |
3 | CO2oc | CO2 from ocean emissions | 44 |
4 | CO2bal | CO2 from balanced biosphere | 44 |
5 | CO2bb | CO2 from biomass burning emissions | 44 |
6 | CO2bf | CO2 from biofuel emissions | 44 |
7 | CO2nte | CO2 from net terrestrial exchange | 44 |
8 | CO2se | CO2 from ship emissions | 44 |
9 | CO2av | CO2 from aircraft emissions | 44 |
10 | CO2ch | CO2 from chemical source | 44 |
11 | CO2corr | CO2 chemical source surface correction | 44 |
For a full tagged CO2 simulation, you can add the following tracers. |
|||
12 | CO2bg | CO2 background (including only fossil fuel CO2) | 44 |
13-52 | CO2xx | CO2 tracers produced in various geographic regions | 44 |
53 | CO2se | CO2 from shipping | 44 |
54 | CO2av | CO2 from aviation | 44 |
Christopher Pickett-Heaps and Kevin Wecht updated the CH4 simulation in GEOS–Chem v8–02–03. Kevin Wecht has further refined the CH4 simulation since then.
For more information, please see:
# | Name | Description | g/mole |
---|---|---|---|
1 | CH4 | Total CH4 | 16 |
2 | CH4og | CH4 produced by oil & gas processing | 16 |
3 | CH4cm | CH4 produced by coal mining | 16 |
4 | CH4ls | CH4 produced by livestock | 16 |
5 | CH4wa | CH4 produced by waste | 16 |
6 | CH4bf | CH4 produced by biofuel | 16 |
7 | CH4ri | CH4 produced by rice | 16 |
8 | CH4an | CH4 produced by other anthropogenic processes | 16 |
9 | CH4bb | CH4 produced by biomass burning | 16 |
10 | CH4we | CH4 produced by wetlands | 16 |
11 | CH4sa | CH4 produced by soil absorption | 16 |
12 | CH4nat | CH4 produced by other natural sources | 16 |
A1.5 Total Hg and Tagged Hg simulations
You can peform the following GEOS–Chem mercury simulations:
For more information, please see:
# | Name | Description | g/mole |
---|---|---|---|
1 | Hg0 | Elemental mercury (total tracer) | 201 |
2 | Hg2 | Divalent mercury (total tracer) | 201 |
3 | HgP | Particulate mercury (total tracer) | 201 |
4 | Hg0_an_na | Elemental Mercury (anthro N. Am. tagged tracer) | 201 |
5 | Hg0_an_eu | Elemental Mercury (anthro Europe tagged tracer) | 201 |
6 | Hg0_an_as | Elemental Mercury (anthro Asia. tagged tracer) | 201 |
7 | Hg0_an_rw | Elemental Mercury (anthro rest-of-world tagged tracer) | 201 |
8 | Hg0_oc | Elemental Mercury (oceanic tagged tracer) | 201 |
9 | Hg0_ln | Elemental Mercury (land re-emission tagged tracer) | 201 |
10 | Hg0_nt | Elemental Mercury (natural land source tagged tracer) | 201 |
11 | Hg2_an_na | Divalent Mercury (anthro N. Am. tagged tracer) | 201 |
12 | Hg2_an_eu | Divalent Mercury (anthro Europe tagged tracer) | 201 |
13 | Hg2_an_as | Divalent Mercury (anthro Asia. tagged tracer) | 201 |
14 | Hg2_an_rw | Divalent Mercury (anthro rest-of-world tagged tracer) | 201 |
15 | Hg2_oc | Divalent Mercury (oceanic tagged tracer) | 201 |
16 | Hg2_ln | Divalent Mercury (land re-emission tagged tracer) | 201 |
17 | Hg2_nt | Divalent Mercury (natural land source tagged tracer) | 201 |
18 | HgP_an_na | Particulate Mercury (anthro N. Am. tagged tracer) | 201 |
19 | HgP_an_eu | Particulate Mercury (anthro Europe tagged tracer) | 201 |
20 | HgP_an_as | Particulate Mercury (anthro Asia. tagged tracer) | 201 |
21 | HgP_an_rw | Particulate Mercury (anthro rest-of-world tagged tracer) | 201 |
22 | HgP_oc | Particulate Mercury (oceanic tagged tracer) | 201 |
23 | HgP_ln | Particulate Mercury (land re-emission tagged tracer) | 201 |
24 | HgP_nt | Particulate Mercury (natural land source tagged tracer) | 201 |
Several GEOS–Chem users have customized the tagged CO simulation to their own purposes. Listed below is the "standard" Tagged CO configuration.
For more information, please see:
# | Name | Description | g/mole |
---|---|---|---|
1 | CO | Total CO | 28 |
2 | COus | CO from US fossil fuel emissions | 28 |
3 | COeur | CO from European fossil fuel emissions | 28 |
4 | COasia | CO from Asian fossil fuel emissions | 28 |
5 | COoth | CO from fossil fuel emissions -- rest of world | 28 |
6 | CObbAm | CO from South American biomass burning | 28 |
7 | CObbAf | CO from African biomass burning | 28 |
8 | CObbAs | CO from SE Asian biomass burning | 28 |
9 | CObbOc | CO from Oceania biomass burning | 28 |
10 | CObbEu | CO from European biomass burning | 28 |
11 | CObbNA | CO from North American biomass burning | 28 |
12 | COch4 | CO chemically produced from methane oxidation | 28 |
13 | CObiof | CO from biofuel burning (whole world) | 28 |
14 | COisop | CO chemically produced from isoprene oxidation | 28 |
15 | COmono | CO chemically produced from monoterpenes oxidation | 28 |
16 | COmeoh | CO chemically produced from methanol oxidation | 28 |
17 | COacet | CO chemically produced from acetone oxidation | 28 |
NOTE: We shall update the tagged Ox simulation in the version following v9–01–03.
For more information, please see:
# | Name | Description | g/mole |
---|---|---|---|
1 | Ox | Total Ox (O3 + NO2 + 2NO3) | 46 |
2 | OxUT | Ox produced in the upper troposphere (above 350 hPa) | 46 |
3 | OxMT | Ox produced in the middle troposphere (PBL top – 350 hPa) | 46 |
4 | OxROW | Ox produced in the rest of the world | 46 |
5 | OxPcBL | Ox produced in the Pacific Ocean boundary layer | 46 |
6 | OxNABL | Ox produced in the North American boundary layer | 46 |
7 | OxAtBL | Ox produced in the Atlantic Ocean boundary layer | 46 |
8 | OxEuBL | Ox produced in the European boundary layer | 46 |
9 | OxAfBL | Ox produced in the African boundary layer | 46 |
10 | OxAsBl | Ox produced in the Asian boundary layer | 46 |
11 | OxStrt | Ox produced in the stratosphere | 46 |
12 | OxInit | Ox from the initial condition | 46 |
13 | OxUSA | Ox produced over the United States (surface – tropopause) | 46 |
We recommend that you run a RnPbBe simulation whenever you modify the convective updraft scavenging or wet deposition algoritms. For more information about this simulation, please see:
# | Name | Description | g/mole |
---|---|---|---|
1 | Rn222 | Radon-222 isotope | 222 |
2 | Pb210 | Lead-210 isotope | 210 |
3 | Be7 | Beryllium-7 isotope | 7 |
The H2/HD simulation has not been used very much recently. If you wish to use this simulation, you will have to invest some time in bringing it back to the state of the science.
# | Name | Description | g/mole |
---|---|---|---|
1 | H2 | Divalent hydrogen | 2 |
2 | HD | Deuterium | 2.0135 |
The CH3I simulation has not been used very much recently. If you wish to use this simulation, you will have to invest some time in bringing it back to the state of the science.
# | Name | Description | g/mole |
---|---|---|---|
1 | CH3I-oc | Methyl iodide from oceans | 141.939 |
2 | CH3I-bb | Methyl iodide from biomass burning | 141.939 |
3 | CH3I-bf | Methyl iodide from biofuel burning | 141.939 |
4 | CH3I-rc | Methyl iodide from rice paddies | 141.939 |
5 | CH3I-wl | Methyl iodide from wetlands | 141.939 |
The HCN simulation has not been used very much recently. If you wish to use this simulation, you will have to invest some time in bringing it back to the state of the science.
# | Name | Description | g/mole |
---|---|---|---|
1 | HCN | Hydrogen Cyanide | 27 |