1.1 Model Intercomparison Project
AerChemMIP
C4MIP
CCMI
CDRMIP
CFMIP
CMIP
CMIP5
CMIP6
CORDEX
DAMIP
DCPP
DECK
DynVarMIP
FAFMIP
GeoMIP
GMMIP
HighResMIP
ISMIP6
LS3MIP
LUMIP
OMIP
PAMIP
PMIP
RFMIP
ScenarioMIP
SIMIP
SPECS
VIACSAB
VolMIP

1.1 Model Intercomparison Project: Chemistry-Climate Model Initiative (CCMI)

Record Label : CCMI

Record Title : Chemistry-Climate Model Initiative

Record identifier : b42b992d-0033-4a54-88c0-ada18f5b141a

Project Home Page : http://www.met.reading.ac.uk/ccmi/

MIP Variable :

Lightning Flash Rate
HCl Volume Mixing Ratio
HNO3 Volume Mixing Ratio
Isoprene Volume Mixing Ratio
Photolysis Rate of NO2
Monthly Loss of Atmospheric Methane
Monthly Loss of Atmospheric Carbon Monoxide
Liquid Water Path
TOA All-Sky Longwave Radiative Forcing Due to Dust
TOA Clear-Sky Longwave Radiative Forcing Due to Aerosols
Maximum PBL Height
Mean Age of Stratospheric Air
Minimum PBL Height
Aerosol Water Mass Mixing Ratio
Elemental Carbon Mass Mixing Ratio
Dust Aerosol Mass Mixing Ratio
NO3 Aerosol Mass Mixing Ratio
Total Organic Aerosol Mass Mixing Ratio
PM1.0 Mass Mixing Ratio
PM10 Mass Mixing Ratio
PM2.5 Mass Mixing Ratio
Secondary Organic Aerosol Mass Mixing Ratio
Sea-Salt Aerosol Mass Mixing Ratio
NO2 Volume Mixing Ratio
Mole Fraction of O3
O3 Destruction Rate
O3 Production Rate
Stratospheric Ozone Tracer Volume Mixing Ratio
Ambient Aerosol Optical Thickness at 440nm
Ambient Aerosol Optical Thickness at 550nm
Aerosol Water Optical Thickness at 550nm
Aerosol Optical Depth at 550nm Due to Biomass Burning
Black Carbon Optical Thickness at 550nm
Dust Optical Thickness at 550nm
Nitrate Aerosol Optical Depth at 550nm
Total Organic Aerosol Optical Depth at 550nm
Sulfate Aerosol Optical Depth at 550nm
Particulate Organic Aerosol Optical Depth at 550nm
Sea-Salt Aerosol Optical Depth at 550nm
OH Volume Mixing Ratio
PAN Volume Mixing Ratio
Photolysis Rate of Ozone (O3) to Excited Atomic Oxygen (the Singlet D State, O1D)
Precipitation
Tropopause Air Pressure
SO2 Volume Mixing Ratio
All-Sky Shortwave Flux Due to Dust at Toa
Clear Sky Shortwave Flux Due to Dust at Toa
Daily Maximum Near-Surface Air Temperature
Daily Minimum Near-Surface Air Temperature
Tropopause Air Temperature
Total Column Ozone
Tropospheric Ozone Column
Air Temperature at Cloud Top
Eastward Wind at 10hPa
Northward Eddy Temperature Flux
Transformed Eulerian Mean Northward Wind
Upward Air Velocity
Wet Deposition Rate of NH3
Wet Deposition Rate of NH4
Wet Deposition Rate of NOy Including Aerosol Nitrate
Transformed Eulerian Mean Upward Wind
Geopotential Height at 10hPa
Geopotential Height at 100hPa
Geopotential Height at 1000hPa
Geopotential Height at 500hPa
Zonal Mean Diabatic Heating Rates
Tropopause Altitude Above Geoid
Vertically Integrated Mass Content of Air in Layer
C2H2 Volume Mixing Ratio
C2H6 Volume Mixing Ratio
Cloud Condensation Nuclei Concentration at Liquid Cloud Top
Aqueous-Phase Production Rate of SO4
Gas-Phase Production Rate of SO4
Total Net Production of Anthropogenic Secondary Organic Aerosol
Convective Cloud Area Percentage
Total Cloud Cover Percentage
Cloud Optical Depth
Tendency of Eastward Wind from Numerical Artefacts
Dry Deposition Rate of Black Carbon Aerosol Mass
Dry Deposition Rate of Dust
Dry Deposition Rate of NH3
Dry Deposition Rate of NH4
Dry Deposition Rate of NOy
Dry Deposition Rate of O3
Dry Deposition Rate of SO2
Dry Deposition Rate of SO4
Dry Deposition Rate of Sea-Salt Aerosol
Total Emission Rate of Anthropogenic CO
Total Emission Rate of Anthropogenic NOx
Total Emission Rate of Anthropogenic Organic Aerosol
Total Emission Rate of Black Carbon Aerosol Mass
Total Emission Rate of Biogenic NMVOC
Total Emission Rate of CO
Total Emission Rate of DMS
Total Emission Rate of Dust
Total Emission Rate of Isoprene
Layer-Integrated Lightning Production of NOx
Total Emission Rate of NH3
Total Emission Rate of NOx
Primary Emission and Chemical Production of Dry Aerosol Organic Matter
Total Emission Rate of SO2
Total Direct Emission Rate of SO4
Total Emission Rate of Sea-Salt Aerosol
Total Emission Rate of NMVOC
Northward Component of the Eliassen-Palm Flux
Upward Component of the Eliassen-Palm Flux