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IPCC Experiments

IPCC ECHAM5-MPI-OM experiments

Name in WDCC 6Hour Monthly Period Description Ident-Name
EH5-T63L31_OM-GR1.5L40_CTL 6H MM 2150-2655 Pre-industrial control experiment PI contrl
EH5-T63L31_OM-GR1.5L40_20C_1
 
EH5-T63L31_OM-GR1.5L40_20C_2
EH5-T63L31_OM-GR1.5L40_20C_3
6H
 
6H
6H
MM
 
MM
MM
1860-2000
 
1860-2000
1860-2000
20th century with anthropogenic forcing (greenhouse gases, sulfate)
initialized in year 2190 of CTL
2. realisation (initialized in year 2215 of CTL)
3. realisation (initialized in year 2240 of CTL)
20C3M
EH5-T63L31_OM-GR1.5L40_20C_1
EH5-T63L31_OM-GR1.5L40_20C_2
EH5-T63L31_OM-GR1.5L40_20C_3
6H
6H
6H
MM
MM
MM
2001-2100
2001-2070
2001-2100
Commitment experiment with constant concentrations (year 2000)
2. realisation
3. realisation
Commit
EH5-T63L31_OM-GR1.5L40_A1B_1
EH5-T63L31_OM-GR1.5L40_A1B_2
EH5-T63L31_OM-GR1.5L40_A1B_3
6H
6H
6H
MM
MM
MM
2001-2100
2001-2100
2001-2100
SRES Szenario: A1B(initialized in year 2000 of 20C_1)
2. realisation (initialized in year 2000 of 20C_2)
3. realisation (initialized in year 2000 of 20C_3)
SRES A1B
EH5-T63L31_OM-GR1.5L40_A1B_1
EH5-T63L31_OM-GR1.5L40_A1B_2
EH5-T63L31_OM-GR1.5L40_A1B_3
6H
6H
6H
MM
MM
MM
2101-2200
2101-2300
2101-2200
Commitment experiment with constant concentrations (year 2100)
2. realisation
3. realisation
Commit
EH5-T63L31_OM-GR1.5L40_B1_1
EH5-T63L31_OM-GR1.5L40_B1_2
EH5-T63L31_OM-GR1.5L40_B1_3
6H
6H
6H
MM
MM
MM
2001-2100
2001-2100
2001-2100
SRES Szenario B1 (initialized in year 2000 of 20C_1)
2. realisation (initialized in year 2000 of 20C_2)
3. realisation (initialized in year 2000 of 20C_3)
SRES B1
EH5-T63L31_OM-GR1.5L40_B1_1
EH5-T63L31_OM-GR1.5L40_B1_2
EH5-T63L31_OM-GR1.5L40_B1_3
6H
6H
6H
MM
MM
MM
2101-2200
2101-2200
2101-2200
Commitment experiment with constant concentrations (year 2100)
2. realisation
3. realisation
Commit
EH5-T63L31_OM-GR1.5L40_A2_1
EH5-T63L31_OM-GR1.5L40_A2_2
EH5-T63L31_OM-GR1.5L40_A2_3
6H
6H
6H
MM
MM
MM
2001-2100
2001-2100
2001-2100
SRES Szenario A2 (initialized in year 2000 of 20C_1)
2. realisation (initialized in year 2000 of 20C_2)
3. realisation (initialized in year 2000 of 20C_3)
SRES A2
EH5-T63L31_OM_1CO2_1
 
 
EH5-T63L31_OM_1CO2_2
EH5-T63L31_OM_1CO2_3
6H
 
 
6H
6H
MM
 
 
MM
MM
1860-1930
 
 
1860-1930
1860-1930
CO2 only: Annual increase of 1% until CO2 doubling w.r.t. CTL in year
1930 (initialized in year 1860 of 20C_1)
All other concentrations like CTL
2. realisation (initialized in year 1860 of 20C_2)
3. realisation (initialized in year 1860 of 20C_3)
1% to 2x
EH5-T63L31_OM_1CO2_1
EH5-T63L31_OM_1CO2_2
EH5-T63L31_OM_1CO2_3
6H
6H
6H
MM
MM
MM
1931-2080
1931-2080
1931-2080
Stabilization at CO2 doubling
2. realisation
3. realisation
 
EH5-T63L31_OM-GR1.5_CMIP4_1
 
EH5-T63L31_OM-GR1.5_CMIP4_1
6H
 
6H
MM
 
MM
1930-2000
 
2001-2188
CO2 only: Annual increase of 1% until CO2 quadrupling w.r.t.
CTL in year 2000 (continuation of 1CO2_2)
Stabilization at CO2 quadrupling
1% to 4x
EH5-T63L31_MLO_CTRL 6H MM 2001-2100 Jan 1978 from AMIP (run 1) including precalculated Q-flux from AMIP (run 1). Well mixed greenhouse gases (CO2, CH4, N2O, F11, F12) are constant (year 1985). Present-day ozone climatology (Fortuin and Kelder, 1998) and background aerosol (Tanre et al., 1984) is applied. Slabcntl
EH5-T63L31_MLO_2CO2 6H MM 2001-2100 Instantaneous CO2 doubling w.r.t. Slbcntl (model years 2001-2100 in database). 2xCO2
EH5-T63L31_AMIP_1
EH5-T63L31_AMIP_2
EH5-T63L31_AMIP_3
6H
6H
6H
MM
MM
MM
1978-1999
1978-1999
1978-1999
Jan. 1978 (observed) for all 3 runs. Initial perturbations in runs 2, 3 are realized by small changes in the horizontal diffusion coefficients during the first month. Well mixed greenhouse gases (CO2, CH4, N2O, F11, F12) are constant (year 1985). Present-day ozone climatology (Fortuin and Kelder, 1998) and background aerosol (Tanre et al., 1984) is applied. AMIP

Comments

  • 'Name' denotes the experiment name in the CERA database
  • 'period' is the time in calendar years for experiments 20C, A1B, B1 und A2. In the experiments CTL, 1CO2 und CMIP4 there is no reference to the calendar. In experiment 1CO2, for example, model year 1930 denotes year 70 (the time of CO2 doubling) after the start of the experiment.
  • 'CTL' is a long control experiment performed under 'pre-industrial' conditions, i.e. the concentrations of well mixed greenhouse gases are fixed at the respective levels of year 1860. No sulfate aerosol is used in CTL. The aim is the reconstruction of a non-drifting climate state representative for the middle of the 19th century as starting point for experiments 20C und 1CO2.
  • The model consists of the atmospheric general circulation model ECHAM5 (Roeckner et al., 2003) in T63L31 resolution and the ocean general circulation model MPI-OM (Marsland et al., 2003) in 1.5°L40 resolution. The models are coupled without flux corrections.
  • Forcing data for transient runs: The concentrations of CO2, CH4, N2O, CFC-11*, CFC-12, O3 and SO4 are prescribed as a function of time (CFC-11* includes the radiative effects of minor CFC's). The long-lived greenhouse gases (CO2 etc.) are prescribed as global annual means. Ozone is prescribed as 2-dimensional distribution (height, latitude) for every month. The 3-dimensional distribution of sulfate aerosol is available every 10 to 20 years as monthly means. The actual concentrations at each grid point and time step are obtained by linear interpolation. Both the direct effect and the 1st indirect (albedo) effect are taken into account.
  • (pdf) Model Information ECHAM5_MPI-OM
latest update: 2008-03-14 10:45