CMIP5 long-term Experiments of MPI-M#
Results of near-term experiments are listed on a separate page: CMIP5 near-term Experiments of MPI-M.
Model: MPI-ESM-LR#
Experiment Name |
Data Access |
Period |
Experiment Description |
Data Citation |
|---|---|---|---|---|
cmip5 output1 MPI-M MPI-ESM-LR amip4xCO2 (MXELa2) |
1979-2008 |
amip4xco2 (6.5 4xCO2 AMIP) - Version 2: Identical to expt. 6.2b, but with AMIP SSTs prescribed as in expt. 3.3 (which is the control for this run). |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The amip4xCO2 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELa2 |
|
cmip5 output1 MPI-M MPI-ESM-LR amip4K (MXELa4) |
1979-2008 |
amip4k (6.8 AMIP plus 4K anomaly) - Version 2: Consistent with CFMIP requirements, add a uniform +4 K SST to the AMIP SSTs of expt. 3.3 (which is the control for this run). |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The amip4K experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELa4 |
|
cmip5 output1 MPI-M MPI-ESM-LR amipFuture (MXELaf) |
1979-2008 |
amipFuture (6.6 AMIP plus patterned anomaly) - Version 2: Consistent with CFMIP requirements, add a patterned SST perturbation to the AMIP SSTs of expt. 3.3 (which is the control for this run). |
Giorgetta et al. (2013): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The amipFuture experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELaf |
|
cmip5 output1 MPI-M MPI-ESM-LR amip (MXELam) |
1979-2008 |
amip (3.3 AMIP) - Version 2: AMIP (1979 - at least 2008). Impose SSTs and sea ice from observations but with other conditions as in experiment 3.2 historical. |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The amip experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELam |
|
cmip5 output1 MPI-M MPI-ESM-LR 1pctCO2 (MXELc1) |
1850-1999 |
1pctCo2 (6.1 1 percent per year CO2) - Version 2: Idealized 1% per year increase in atmospheric CO2 to quadrupling. |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The 1pctCO2 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELc1 |
|
cmip5 output2 MPI-M MPI-ESM-LR 1pctCO2 (MXELc12) |
Giorgetta et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR 1pctCO2, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXELc12 |
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cmip5 output1 MPI-M MPI-ESM-LR abrupt4xCO2 (MXELc2) |
1850-1999 |
abrupt4xco2 (6.3 Abrupt 4XCO2) - Version 2: Impose an instantaneous quadrupling of CO2, then hold fixed. |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The abrupt4xCO2 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELc2 |
|
cmip5 output2 MPI-M MPI-ESM-LR abrupt4xCO2 (MXELc22) |
Giorgetta et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR abrupt4xCO2, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXELc22 |
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cmip5 output1 MPI-M MPI-ESM-LR esmFdbk1 (MXELe1) |
1850-1999 |
esmFdbk1 (5.5-1 ESM feedback 1) - Version 2: Impose conditions identical to 3.1::Control but radiation code sees CO2 concentration increase. |
Reick et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The esmFdbk1 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELe1 |
|
cmip5 output2 MPI-M MPI-ESM-LR esmFdbk1 (MXELe12) |
Reick et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR esmFdbk1, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXELe12 |
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cmip5 output1 MPI-M MPI-ESM-LR esmFixClim1 (MXELx1) |
1850-1999 |
esmFixClim1 (5.4-1 ESM fixed climatem 1) - Version 2: Impose conditions identical to experiment 3.1 but the carbon cycle sees CO2 concentration increase. |
Reick et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The esmFixClim1 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELx1 |
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cmip5 output2 MPI-M MPI-ESM-LR esmFixClim1 (MXELx12) |
Reick et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR esmFixClim1, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXELx12 |
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cmip5 output1 MPI-M MPI-ESM-LR esmrcp85 (MXELe8) |
2006-2100 |
esmrcp85 (5.3 ESM RCP8.5) - Version 2: Future projection (2006-2100) forced by RCP8.5. As in experiment 4.2_RCP8.5 but emissions-forced (with atmospheric CO2 determined by the model itself). |
Reick et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The esmrcp85 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELe8 |
|
cmip5 output2 MPI-M MPI-ESM-LR esmrcp85 (MXELe82) |
Reick et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR esmrcp85, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXELe82 |
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cmip5 output1 MPI-M MPI-ESM-LR esmControl (MXELec) |
1850-2849 |
esmControl (5.1 ESM pre-industrial control) - Version 2: Impose non-evolving pre-industrial conditions as in experiment 3.1_piControl but emissions-forced (with atmosperhic CO2 determined by the model itself) |
Reick et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The esmControl experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELec |
|
cmip5 output2 MPI-M MPI-ESM-LR esmControl (MXELec2) |
Reick et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR esmControl, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXELec2 |
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cmip5 output1 MPI-M MPI-ESM-LR esmHistorical (MXELeh) |
1850-2005 |
esmHistorical (5.2 ESM historical) - Version 2: Historical simulation (1850 to 2005) as in experiment 3.2_historical but emissions-forced (with atmospheric CO2 determined by the model itself) |
Reick et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The esmHistorical experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELeh |
|
cmip5 output2 MPI-M MPI-ESM-LR esmHistorical (MXELeh2) |
Reick et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR esmHistorical, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXELeh2 |
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cmip5 output1 MPI-M MPI-ESM-LR historical (MXELhi) |
1850-2005 |
historical (3.2 Historical) - Version 2: Simulation of recent past (1850 to 2005). Impose changing conditions (consistent with observations). |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The historical experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELhi |
|
cmip5 output2 MPI-M MPI-ESM-LR historical (MXELhi2) |
Giorgetta et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR historical, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXELhi2 |
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cmip5 output1 MPI-M MPI-ESM-LR piControl (MXELpc) |
1850-2849 |
piControl (3.1 Pre-Industrial Control) - Version 3: Pre-Industrial coupled atmosphere/ocean control run. Imposes non-evolving pre-industrial conditions. |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The piControl experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELpc |
|
cmip5 output2 MPI-M MPI-ESM-LR piControl (MXELpc2) |
Giorgetta et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR piControl, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXELpc2 |
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cmip5 output1 MPI-M MPI-ESM-LR aqua4xCO2 (MXELq2) |
1979-1983 |
aqua4xco2 (6.7b 4xCO2 aqua planet) - Version 2: Consistent with CFMIP requirements, impose a 4xCO2 on zonally uniform SSTs of expt. 6.7a (which is the control for this run). |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The aqua4xCO2 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELq2 |
|
cmip5 output1 MPI-M MPI-ESM-LR aqua4K (MXELq4) |
1979-1983 |
aqua4k (6.7c aqua planet plus 4K anomaly) - Version 2: Consistent with CFMIP requirements, add a uniform +4K to the zonally uniform SSTs of expt. 6.7a (which is the control for this run). |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The aqua4K experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELq4 |
|
cmip5 output1 MPI-M MPI-ESM-LR aquaControl (MXELqc) |
1979-1983 |
aquaControl (6.7a aqua planet control) - Version 2: Consistent with CFMIP requirements, impose zonally uniform SSTs on a planet without continents. |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The aquaControl experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELqc |
|
cmip5 output1 MPI-M MPI-ESM-LR rcp26 (MXELr2) |
2006-2300 |
rcp26 (4.3 RCP2.6) - Version 2: Future projection (2006-2100) forced by RCP2.6. RCP2.6 is a representative concentration pathway which approximately results in a radiative forcing of 2.6 W m-2 at year 2100, relative to pre-industrial conditions. |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The rcp26 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELr2 |
|
cmip5 output2 MPI-M MPI-ESM-LR rcp26 (MXELr22) |
Giorgetta et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR rcp26, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXELr22 |
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cmip5 output1 MPI-M MPI-ESM-LR rcp45 (MXELr4) |
2006-2300 |
rcp45 (4.1 RCP4.5) - Version 2: Future projection (2006-2100) forced by RCP4.5. RCP4.5 is a representative concentration pathway which approximately results in a radiative forcing of 4.5 W m-2 at year 2100, relative to pre-industrial conditions. RCPs are time-dependent, consistent projections of emissions and concentrations of radiatively active gases and particles. |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The rcp45 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELr4 |
|
cmip5 output2 MPI-M MPI-ESM-LR rcp45 (MXELr42) |
Giorgetta et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR rcp45, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXELr42 |
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cmip5 output1 MPI-M MPI-ESM-LR rcp85 (MXELr8) |
2006-2300 |
rcp85 (4.2 RCP8.5) - Version 2: Future projection (2006-2100) forced by RCP8.5. RCP8.5 is a representative concentration pathway which approximately results in a radiative forcing of 8.5 W m-2 at year 2100, relative to pre-industrial conditions. RCPs are time-dependent, consistent projections of emissions and concentrations of radiatively active gases and particles. |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The rcp85 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELr8 |
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cmip5 output2 MPI-M MPI-ESM-LR rcp85 (MXELr82) |
Giorgetta et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR rcp85, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXELr82 |
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cmip5 output1 MPI-M MPI-ESM-LR sstClim4xCO2 (MXELs2) |
1850-1879 |
sstClim4xco2 (6.2b SST Climatology With 4XCO2 Forcing) - Version 2: AMIP-style experiment with control run climatological SSTs and sea ice (as in 6.2a) but with quadrupled 4XCO2 imposed. |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The sstClim4xCO2 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELs2 |
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cmip5 output1 MPI-M MPI-ESM-LR sstClim (MXELsc) |
1850-1879 |
sstClim (6.2a Control SST Climatology) - Version 2: AMIP-style experiment with control run climatological SSTs and sea ice. |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The sstClim experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELsc |
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cmip5 output1 MPI-M MPI-ESM-LR sstClimAerosol (MXELsa) |
1850-1879 |
6.4a sstClimAerosol (6.4a all aerosol forcing) - Version 1: AMIP-style experiment with control run climatological SSTs and sea ice (as in expt. 6.2a) but with aerosols consistent with conditions in year 2000 of the historical run (expt. 3.2) |
Giorgetta et al. (2014): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The sstClimAerosol experiment, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXELsa |
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cmip5 output1 MPI-M MPI-ESM-LR sstClimSulfate (MXELss) |
1850-1879 |
6.4b sstClimSulfate (6.4b sulfate aerosol forcing) - Version 1: AMIP-style experiment with control run climatological SSTs and sea ice (as in expt. 6.2a) but with aerosols consistent with conditions in year 2000 of the historical run (expt. 3.2) |
Giorgetta et al. (2014): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The sstClimSulfate experiment, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXELss |
Model: MPI-ESM-MR#
Experiment Name |
Data Access |
Period |
Experiment Description |
Data Citation |
|---|---|---|---|---|
cmip5 output1 MPI-M MPI-ESM-MR amip4xCO2 (MXMRa2) |
1979-2008 |
amip4xco2 (6.5 4xCO2 AMIP) - Version 2: Identical to expt. 6.2b, but with AMIP SSTs prescribed as in expt. 3.3 (which is the control for this run). |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The amip4xCO2 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMRa2 |
|
cmip5 output1 MPI-M MPI-ESM-MR amip4K (MXMRa4) |
1979-2008 |
amip4k (6.8 AMIP plus 4K anomaly) - Version 2: Consistent with CFMIP requirements, add a uniform +4 K SST to the AMIP SSTs of expt. 3.3 (which is the control for this run). |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The amip4K experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMRa4 |
|
cmip5 output1 MPI-M MPI-ESM-MR amipFuture (MXMRaf) |
1979-2008 |
amipFuture (6.6 AMIP plus patterned anomaly) - Version 2: Consistent with CFMIP requirements, add a patterned SST perturbation to the AMIP SSTs of expt. 3.3 (which is the control for this run). |
Giorgetta et al. (2013): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The amipFuture experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMRaf |
|
cmip5 output1 MPI-M MPI-ESM-MR amip (MXMRam) |
1979-2008 |
amip (3.3 AMIP) - Version 2: AMIP (1979 - at least 2008). Impose SSTs and sea ice from observations but with other conditions as in experiment 3.2 historical. |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The amip experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMRam |
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cmip5 output1 MPI-M MPI-ESM-MR 1pctCO2 (MXMRc1) |
1850-1999 |
1pctCo2 (6.1 1 percent per year CO2) - Version 2: Idealized 1% per year increase in atmospheric CO2 to quadrupling. |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The 1pctCO2 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMRc1 |
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cmip5 output2 MPI-M MPI-ESM-MR 1pctCO2 (MXMRc12) |
Giorgetta et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR 1pctCO2, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMRc12 |
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cmip5 output1 MPI-M MPI-ESM-MR abrupt4xCO2 (MXMRc2) |
1850-1999 |
abrupt4xco2 (6.3 Abrupt 4XCO2) - Version 2: Impose an instantaneous quadrupling of CO2, then hold fixed. |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The abrupt4xCO2 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMRc2 |
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cmip5 output2 MPI-M MPI-ESM-MR abrupt4xCO2 (MXMRc22) |
Giorgetta et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR abrupt4xCO2, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMRc22 |
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cmip5 output1 MPI-M MPI-ESM-MR historical (MXMRhi) |
1850-2005 |
historical (3.2 Historical) - Version 2: Simulation of recent past (1850 to 2005). Impose changing conditions (consistent with observations). |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The historical experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMRhi |
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cmip5 output2 MPI-M MPI-ESM-MR historical (MXMRhi2) |
Giorgetta et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR historical, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMRhi2 |
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cmip5 output1 MPI-M MPI-ESM-MR piControl (MXMRpc) |
1850-2849 |
piControl (3.1 Pre-Industrial Control) - Version 3: Pre-Industrial coupled atmosphere/ocean control run. Imposes non-evolving pre-industrial conditions. |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The piControl experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMRpc |
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cmip5 output2 MPI-M MPI-ESM-MR piControl (MXMRpc2) |
Giorgetta et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR piControl, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMRpc2 |
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cmip5 output1 MPI-M MPI-ESM-MR aqua4xCO2 (MXMRq2) |
1979-1983 |
aqua4xco2 (6.7b 4xCO2 aqua planet) - Version 2: Consistent with CFMIP requirements, impose a 4xCO2 on zonally uniform SSTs of expt. 6.7a (which is the control for this run). |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The aqua4xCO2 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMRq2 |
|
cmip5 output1 MPI-M MPI-ESM-MR aqua4K (MXMRq4) |
1979-1983 |
aqua4k (6.7c aqua planet plus 4K anomaly) - Version 2: Consistent with CFMIP requirements, add a uniform +4K to the zonally uniform SSTs of expt. 6.7a (which is the control for this run). |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The aqua4K experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMRq4 |
|
cmip5 output1 MPI-M MPI-ESM-MR aquaControl (MXMRqc) |
1979-1983 |
aquaControl (6.7a aqua planet control) - Version 2: Consistent with CFMIP requirements, impose zonally uniform SSTs on a planet without continents. |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The aquaControl experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMRqc |
|
cmip5 output1 MPI-M MPI-ESM-MR rcp26 (MXMRr2) |
2006-2100 |
rcp26 (4.3 RCP2.6) - Version 2: Future projection (2006-2100) forced by RCP2.6. RCP2.6 is a representative concentration pathway which approximately results in a radiative forcing of 2.6 W m-2 at year 2100, relative to pre-industrial conditions. |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The rcp26 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMRr2 |
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cmip5 output2 MPI-M MPI-ESM-MR rcp26 (MXMRr22) |
Giorgetta et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR rcp26, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMRr22 |
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cmip5 output1 MPI-M MPI-ESM-MR rcp45 (MXMRr4) |
2006-2100 |
rcp45 (4.1 RCP4.5) - Version 2: Future projection (2006-2100) forced by RCP4.5. RCP4.5 is a representative concentration pathway which approximately results in a radiative forcing of 4.5 W m-2 at year 2100, relative to pre-industrial conditions. RCPs are time-dependent, consistent projections of emissions and concentrations of radiatively active gases and particles. |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The rcp45 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMRr4 |
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cmip5 output2 MPI-M MPI-ESM-MR rcp45 (MXMRr42) |
Giorgetta et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR rcp45, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMRr42 |
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cmip5 output1 MPI-M MPI-ESM-MR rcp85 (MXMRr8) |
2006-2100 |
rcp85 (4.2 RCP8.5) - Version 2: Future projection (2006-2100) forced by RCP8.5. RCP8.5 is a representative concentration pathway which approximately results in a radiative forcing of 8.5 W m-2 at year 2100, relative to pre-industrial conditions. RCPs are time-dependent, consistent projections of emissions and concentrations of radiatively active gases and particles. |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The rcp85 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMRr8 |
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cmip5 output2 MPI-M MPI-ESM-MR rcp85 (MXMRr82) |
Giorgetta et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR rcp85, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMRr82 |
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cmip5 output1 MPI-M MPI-ESM-MR sstClim4xCO2 (MXMRs2) |
1850-1879 |
sstClim4xco2 (6.2b SST Climatology With 4XCO2 Forcing) - Version 2: AMIP-style experiment with control run climatological SSTs and sea ice (as in 6.2a) but with quadrupled 4XCO2 imposed. |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The sstClim4xCO2 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMRs2 |
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cmip5 output1 MPI-M MPI-ESM-MR sstClim (MXMRsc) |
1850-1879 |
sstClim (6.2a Control SST Climatology) - Version 2: AMIP-style experiment with control run climatological SSTs and sea ice. |
Giorgetta et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The sstClim experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMRsc |
Model: MPI-ESM-P#
Experiment Name |
Data Access |
Period |
Experiment Description |
Data Citation |
|---|---|---|---|---|
cmip5 output1 MPI-M MPI-ESM-P 1pctCO2 (MXEPc1) |
1850-1989 |
1pctCo2 (6.1 1 percent per year CO2) - Version 2: Idealized 1% per year increase in atmospheric CO2 to quadrupling. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-P model: The 1pctCO2 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXEPc1 |
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cmip5 output2 MPI-M MPI-ESM-P 1pctCO2 (MXEPc12) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-P 1pctCO2, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEPc12 |
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cmip5 output1 MPI-M MPI-ESM-P abrupt4xCO2 (MXEPc2) |
1850-1999 |
abrupt4xco2 (6.3 Abrupt 4XCO2) - Version 2: Impose an instantaneous quadrupling of CO2, then hold fixed. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-P model: The abrupt4xCO2 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXEPc2 |
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cmip5 output2 MPI-M MPI-ESM-P abrupt4xCO2 (MXEPc22) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-P abrupt4xCO2, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEPc22 |
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cmip5 output1 MPI-M MPI-ESM-P historical (MXEPhi) |
1850-2005 |
historical (3.2 Historical) - Version 2: Simulation of recent past (1850 to 2005). Impose changing conditions (consistent with observations). |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-P model: The historical experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXEPhi |
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cmip5 output2 MPI-M MPI-ESM-P historical (MXEPhi2) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-P historical, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEPhi2 |
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cmip5 output1 MPI-M MPI-ESM-P lgm (MXEPlg) |
1850-1949 |
lgm (3.5 Last glacial maximum) - Version 2: Consistent with PMIP (Paleo Model Intercomparison Project) requirements. Impose Last Glacial Maximum (21 kyrs ago) conditions including ice sheets and atmospheric concentrations of well-mixed greenhouse gasses. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-P model: The lgm experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXEPlg |
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cmip5 output2 MPI-M MPI-ESM-P lgm (MXEPlg2) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-P lgm, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEPlg2 |
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cmip5 output1 MPI-M MPI-ESM-P midHolocene (MXEPmh) |
1850-1949 |
midHolocene (3.4 mid-Holocene) - Version 2: Consistent with PMIP (Paleo Model Intercomparison Project) specifications. Impose Mid-Holocene (6 kyrs ago) conditions including Orbital parameters and Atmospheric concentrations of well-mixed greenhouse gasses. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-P model: The midHolocene experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXEPmh |
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cmip5 output2 MPI-M MPI-ESM-P midHolocene (MXEPmh2) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-P midHolocene, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEPmh2 |
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cmip5 output1 MPI-M MPI-ESM-P piControl (MXEPpc) |
1850-3005 |
piControl (3.1 Pre-Industrial Control) - Version 3: Pre-Industrial coupled atmosphere/ocean control run. Imposes non-evolving pre-industrial conditions. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-P model: The piControl experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXEPpc |
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cmip5 output2 MPI-M MPI-ESM-P piControl (MXEPpc2) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-P piControl, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEPpc2 |
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cmip5 output1 MPI-M MPI-ESM-P past1000 (MXEPpk) |
850-1849 |
past1000 (3.6 Last millennium) - Version 2: Consistent with PMIP (Paleo Model Intercomparison Project) requirements, Impose evolving conditions including: Solar Variations and Volcanic Aerosols. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-P model: The past1000 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXEPpk |
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cmip5 output2 MPI-M MPI-ESM-P past1000 (MXEPpk2) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-P past1000, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEPpk2 |
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cmip5 output1 MPI-M MPI-ESM-P sstClim4xCO2 (MXEPs2) |
1850-1879 |
sstClim4xco2 (6.2b SST Climatology With 4XCO2 Forcing) - Version 2: AMIP-style experiment with control run climatological SSTs and sea ice (as in 6.2a) but with quadrupled 4XCO2 imposed. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-P model: The sstClim4xCO2 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXEPs2 |
|
cmip5 output1 MPI-M MPI-ESM-P sstClim (MXEPsc) |
1850-1879 |
sstClim (6.2a Control SST Climatology) - Version 2: AMIP-style experiment with control run climatological SSTs and sea ice. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-P model: The sstClim experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXEPsc |
Comments
‘Experiment Name’: The CMIP5 experiment name (DRS) and the acronyms used within the CERA database are given.
‘output1/output2’: CMIP5 data was collected in two products. output1 data was viewed as more important and replicated among the CMIP5 Archive centers at PCMDI, BADC and DKRZ. output2 data can be viewed as an extention of the output1 data, which was archived at DKRZ only for MPI-M data.
‘period’ is the time in calendar years for experiments historical, rcp*, lgm, midHolocene, and past1000. In the experiments piControl, 1pctCO2, abrupt4xCO2, sstClim* there is no reference to the calendar.