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  • Using CAM-chem Output
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CAM-chem output is saved as gridded files. Finite volume simulations use a regular grid.

Time: Instantaneous time saves exactly at the time specified. Average time saves at the end of the time period. For example a month average of January 1 to 31 will save at midnight on January 31.

Altitude: Vertical layers are sigma hybrid coordinates. You can convert into layer centers or edge pressures using the conversion factors (P0, hyam/hyai, hybm/hybi) combined with surface pressure. NCL has an example of converting hybrid to pressure coordinates:  The variable 'Z3' contains altitude in m.

Horizontal resolution: Latitude and longitude coordinates are saved and represent center values of the grid box.

An overview describing CESM output in general and suggesting some options for visualization and analysis can be found in the following lecture notes:

Unidata has some great python examples for atmospheric science:

CAM-chem specific python examples will be found here:

MUSICA is developing some visualization tool examples under "viewing output":

Explanations of output diagnostic variables

Output variableUnitsDefinition
SF_<species>kg/m2/sEmissions of species (Surface Flux)
MEG_<species>kg/m2/sBiogenic emissions calculated by MEGAN in CLM
LNO_PRODmolecules /cm3/s3D lightning NO emissions
vertically integrated lightning NO emissions

Dry Deposition Velocity of species

DF_<species>kg/m2/sDry Deposition Flux of species
DTWR_<species>kg/kg/sWashout Rate of species (3D field)
WD_<species>kg/m2/sWet Deposition vertically integrated flux. Note: prior to CESM2 this was output in units (kg/grid-box/s).



molecules /cm3/sTotal chemical production and loss for species (based on equations found in $CASE/CaseDocs/chem_mech.doc).  



molecules /cm3/s

For ozone, the gross production and loss terms (CHMP, CHML) are not particularly useful as they include the fast cycling reactions, so O3_Prod and O3_Loss are defined to represent the sum of the rate-limiting reactions of the OddOx family (O3 + O + O1D + NO2).  These are the key terms in the OddOx equations. In hindsight, these O3_Prod and O3_Loss names probably should not have the name O3_ in them. These reactions are aimed primarily at deriving the tropospheric photochemical smog chemistry. The main reactions are:

O3_Prod = NO_HO2 + CH3O2_NO + PO2_NO + CH3CO3_NO + C2H5O2_NO + .92*ISOPAO2_NO + .92*ISOPBO2_NO + MACRO2_NOa + MCO3_NO + C3H7O2_NO + RO2_NO + XO2_NO + .9*TOLO2_NO + .9*PHENO2_NO + .9*C6H5O2_NO + .9*BENZO2_NO + .9*MALO2_NO + .9*BZOO_NO + .9*ACBZO2_NO + .9*DICARBO2_NO + .9*MDIALO2_NO  + .9*XYLOLO2_NO + .9*XYLENO2_NO + TERPO2_NO + TERP2O2_NO + NTERPO2_NO + ALKO2_NO + ENEO2_NO +  EO2_NO + MEKO2_NO + HOCH2OO_NO + jonitr

O3_Loss = O1D_H2O + OH_O3 + HO2_O3 + H_O3 + C3H6_O3 + .9*ISOP_O3 + C2H4_O3 + .8*MVK_O3 + 0.8*MACR_O3 + MTERP_O3 + BCARY_O3

These diagnostic terms are now (CESM2) defined in the atm_in namelist (the rxn_rate_sums variable in the rxn_rates_diag_nl group).  These rate sums can be modified, or additional ones created, by the user in user_nl_cam.  

j<photorate_label>/sPhotolysis rate constant
r_j<photorate_label>molecules /cm3/sPhotolysis rate (j * species density)
Reaction rate constant (e.g., "O1D_H2O" gives k for O1D+H2O)
r_<rxnrate_label>molecules /cm3/sReaction rate (k * [O1D] * [H2O] )

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