CMIP5 near-term Experiments of MPI-M#
Results of long-term experiments are listed on a separate page: CMIP5 long-term Experiments of MPI-M.
Model: MPI-ESM-LR#
Experiment Name |
Data Access |
Period |
Description |
Data Citation |
|---|---|---|---|---|
cmip5 output1 MPI-M MPI-ESM-LR decadals (MXELDEC) |
1961-2035 |
decadalYYYY (10-year/30-year hindcast/prediction initialized in year YYYY) - Version 2: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2013): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The decadal experiments, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELDEC |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1960 (MXEL60) |
1961-1990 |
decadal1960 (30-year hindcast/prediction initialized in year 1960) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The decadal1960 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXEL60 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1960 (MXEL602) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1960, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL602 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1961 (MXEL61) |
1962-1971 |
decadal1961 (10-year hindcast/prediction initialized in year 1961) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1961, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL61 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1961 (MXEL612) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1961, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL612 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1962 (MXEL62) |
1963-1972 |
decadal1962 (10-year hindcast/prediction initialized in year 1962) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1962, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL62 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1962 (MXEL622) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1962, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL622 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1963 (MXEL63) |
1964-1973 |
decadal1963 (10-year hindcast/prediction initialized in year 1963) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1963, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL63 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1963 (MXEL632) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1963, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL632 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1964 (MXEL64) |
1965-1974 |
decadal1964 (10-year hindcast/prediction initialized in year 1964) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1964, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL64 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1964 (MXEL642) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1964, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL642 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1965 (MXEL65) |
1966-1975 |
decadal1965 (10-year hindcast/prediction initialized in year 1965) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The decadal1965 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXEL65 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1965 (MXEL652) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1965, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL652 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1966 (MXEL66) |
1967-1976 |
decadal1966 (10-year hindcast/prediction initialized in year 1966) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1966, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL66 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1966 (MXEL662) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1966, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL662 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1967 (MXEL67) |
1968-1977 |
decadal1967 (10-year hindcast/prediction initialized in year 1967) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1967, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL67 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1967 (MXEL672) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1967, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL672 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1968 (MXEL68) |
1969-1978 |
decadal1968 (10-year hindcast/prediction initialized in year 1968) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1968, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL68 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1968 (MXEL682) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1968, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL682 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1969 (MXEL69) |
1970-1979 |
decadal1969 (10-year hindcast/prediction initialized in year 1969) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1969, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL69 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1969 (MXEL692) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1969, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL692 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1970 (MXEL70) |
1971-1980 |
decadal1970 (10-year hindcast/prediction initialized in year 1970) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The decadal1970 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXEL70 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1970 (MXEL702) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1970, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL702 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1971 (MXEL71) |
1972-1981 |
decadal1971 (10-year hindcast/prediction initialized in year 1971) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1971, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL71 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1971 (MXEL712) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1971, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL712 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1972 (MXEL72) |
1973-1982 |
decadal1972 (10-year hindcast/prediction initialized in year 1972) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1972, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL72 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1972 (MXEL722) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1972, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL722 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1973 (MXEL73) |
1974-1983 |
decadal1973 (10-year hindcast/prediction initialized in year 1973) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1973, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL73 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1973 (MXEL732) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1973, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL732 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1974 (MXEL74) |
1975-1984 |
decadal1974 (10-year hindcast/prediction initialized in year 1974) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1974, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL74 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1974 (MXEL742) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1974, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL742 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1975 (MXEL75) |
1976-1985 |
decadal1975 (10-year hindcast/prediction initialized in year 1975) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The decadal1975 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXEL75 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1975 (MXEL752) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1975, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL752 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1976 (MXEL76) |
1977-1986 |
decadal1976 (10-year hindcast/prediction initialized in year 1976) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1976, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL76 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1976 (MXEL762) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1976, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL762 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1977 (MXEL77) |
1978-1987 |
decadal1977 (10-year hindcast/prediction initialized in year 1977) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1977, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL77 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1977 (MXEL772) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1977, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL772 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1978 (MXEL78) |
1979-1988 |
decadal1978 (10-year hindcast/prediction initialized in year 1978) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1978, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL78 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1978 (MXEL782) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1978, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL782 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1979 (MXEL79) |
1980-1989 |
decadal1979 (10-year hindcast/prediction initialized in year 1979) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1979, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL79 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1979 (MXEL792) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1979, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL792 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1980 (MXEL80) |
1981-2010 |
decadal1980 (30-year hindcast/prediction initialized in year 1980) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The decadal1980 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXEL80 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1980 (MXEL802) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1980, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL802 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1981 (MXEL81) |
1982-1991 |
decadal1981 (10-year hindcast/prediction initialized in year 1981) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1981, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL81 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1981 (MXEL812) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1981, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL812 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1982 (MXEL82) |
1983-1992 |
decadal1982 (10-year hindcast/prediction initialized in year 1982) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1982, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL82 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1982 (MXEL822) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1982, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL822 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1983 (MXEL83) |
1984-1993 |
decadal1983 (10-year hindcast/prediction initialized in year 1983) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1983, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL83 |
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cmip5 output2 MPI-M MPI-ESM-LR decadal1983 (MXEL832) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1983, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL832 |
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cmip5 output1 MPI-M MPI-ESM-LR decadal1984 (MXEL84) |
1985-1994 |
decadal1984 (10-year hindcast/prediction initialized in year 1984) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1984, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL84 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal1984 (MXEL842) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1984, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL842 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal1985 (MXEL85) |
1986-1995 |
decadal1985 (10-year hindcast/prediction initialized in year 1985) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The decadal1985 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXEL85 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal1985 (MXEL852) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1985, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL852 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal1986 (MXEL86) |
1987-1996 |
decadal1986 (10-year hindcast/prediction initialized in year 1986) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1986, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL86 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal1986 (MXEL862) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1986, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL862 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal1987 (MXEL87) |
1988-1997 |
decadal1987 (10-year hindcast/prediction initialized in year 1987) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1987, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL87 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal1987 (MXEL872) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1987, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL872 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal1988 (MXEL88) |
1989-1998 |
decadal1988 (10-year hindcast/prediction initialized in year 1988) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1988, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL88 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal1988 (MXEL882) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1988, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL882 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal1989 (MXEL89) |
1990-1999 |
decadal1989 (10-year hindcast/prediction initialized in year 1989) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1989, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL89 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal1989 (MXEL892) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1989, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL892 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal1990 (MXEL90) |
1991-2000 |
decadal1990 (10-year hindcast/prediction initialized in year 1990) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The decadal1990 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXEL90 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal1990 (MXEL902) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1990, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL902 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal1991 (MXEL91) |
1992-2001 |
decadal1991 (10-year hindcast/prediction initialized in year 1991) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1991, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL91 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal1991 (MXEL912) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1991, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL912 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal1992 (MXEL92) |
1993-2002 |
decadal1992 (10-year hindcast/prediction initialized in year 1992) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1992, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL92 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal1992 (MXEL922) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1992, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL922 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal1993 (MXEL93) |
1994-2003 |
decadal1993 (10-year hindcast/prediction initialized in year 1993) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1993, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL93 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal1993 (MXEL932) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1993, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL932 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal1994 (MXEL94) |
1995-2004 |
decadal1994 (10-year hindcast/prediction initialized in year 1994) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1994, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL94 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal1994 (MXEL942) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1994, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL942 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal1995 (MXEL95) |
1996-2005 |
decadal1995 (10-year hindcast/prediction initialized in year 1995) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The decadal1995 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXEL95 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal1995 (MXEL952) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1995, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL952 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal1996 (MXEL96) |
1997-2006 |
decadal1996 (10-year hindcast/prediction initialized in year 1996) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1996, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL96 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal1996 (MXEL962) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1996, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL962 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal1997 (MXEL97) |
1998-2007 |
decadal1997 (10-year hindcast/prediction initialized in year 1997) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1997, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL97 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal1997 (MXEL972) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1997, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL972 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal1998 (MXEL98) |
1999-2008 |
decadal1998 (10-year hindcast/prediction initialized in year 1998) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1998, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL98 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal1998 (MXEL982) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1998, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL982 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal1999 (MXEL99) |
2000-2009 |
decadal1999 (10-year hindcast/prediction initialized in year 1999) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal1999, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL99 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal1999 (MXEL992) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal1999, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL992 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal2000 (MXEL00) |
2001-2010 |
decadal2000 (10-year hindcast/prediction initialized in year 2000) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The decadal2000 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXEL00 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal2000 (MXEL002) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal2000, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL002 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal2001 (MXEL01) |
2002-2011 |
decadal2001 (10-year hindcast/prediction initialized in year 2001) - Version 2: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal2001, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL01 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal2001 (MXEL012) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal2001, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL012 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal2002 (MXEL02) |
2003-2012 |
decadal2002 (10-year hindcast/prediction initialized in year 2002) - Version 2: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal2002, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL02 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal2002 (MXEL022) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal2002, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL022 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal2003 (MXEL03) |
2004-2013 |
decadal2003 (10-year hindcast/prediction initialized in year 2003) - Version 2: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal2003, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL03 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal2003 (MXEL032) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal2003, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL032 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal2004 (MXEL04) |
2005-2014 |
decadal2004 (10-year hindcast/prediction initialized in year 2004) - Version 2: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal2004, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL04 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal2004 (MXEL042) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal2004, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL042 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal2005 (MXEL05) |
2006-2035 |
decadal2005 (30-year hindcast/prediction initialized in year 2005) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The decadal2005 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXEL05 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal2005 (MXEL052) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal2005, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL052 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal2006 (MXEL06) |
2007-2016 |
decadal2006 (10-year hindcast/prediction initialized in year 2006) - Version 2: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal2006, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL06 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal2006 (MXEL062) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal2006, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL062 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal2007 (MXEL07) |
2008-2017 |
decadal2007 (10-year hindcast/prediction initialized in year 2007) - Version 2: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal2007, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL07 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal2007 (MXEL072) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal2007, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL072 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal2008 (MXEL08) |
2009-2018 |
decadal2008 (10-year hindcast/prediction initialized in year 2008) - Version 2: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal2008, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL08 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal2008 (MXEL082) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal2008, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL082 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal2009 (MXEL09) |
2010-2019 |
decadal2009 (10-year hindcast/prediction initialized in year 2009) - Version 2: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-LR decadal2009, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL09 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal2009 (MXEL092) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal2009, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL092 |
|||
cmip5 output1 MPI-M MPI-ESM-LR decadal2010 (MXEL10) |
2011-2020 |
decadal2010 (10-year hindcast/prediction initialized in year 2010) - Version 2: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The decadal2010 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXEL10 |
|
cmip5 output2 MPI-M MPI-ESM-LR decadal2010 (MXEL102) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR decadal2010, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXEL102 |
|||
cmip5 output1 MPI-M MPI-ESM-LR noVolc1960 (MXELv6) |
1961-1970 |
noVolc1960 (1.3 hindcast without volcanoes (1960)) - Version 3: Hindcast without volcanoes. Additional 10yr run for experiment 1.1 from 1960 without including the Agung, El Chichon and Pinatubo eruptions. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The noVolc1960 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELv6 |
|
cmip5 output2 MPI-M MPI-ESM-LR noVolc1960 (MXELv62) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR noVolc1960, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXELv62 |
|||
cmip5 output1 MPI-M MPI-ESM-LR noVolc1975 (MXELv7) |
1976-1985 |
noVolc1975 (1.3 hindcast without volcanoes (1975)) - Version 3: Hindcast without volcanoes. Additional 10yr run for experiment 1.1 from 1975 without including the Agung, El Chichon and Pinatubo eruptions. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The noVolc1975 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELv7 |
|
cmip5 output2 MPI-M MPI-ESM-LR noVolc1975 (MXELv72) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR noVolc1975, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXELv72 |
|||
cmip5 output1 MPI-M MPI-ESM-LR noVolc1980 (MXELv0) |
1981-1990 |
noVolc1980 (1.3 hindcast without volcanoes (1980)) - Version 3: Hindcast without volcanoes. Additional 10yr run for experiment 1.1 from 1980 without including the Agung, El Chichon and Pinatubo eruptions. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The noVolc1980 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELv0 |
|
cmip5 output2 MPI-M MPI-ESM-LR noVolc1980 (MXELv02) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR noVolc1980, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXELv02 |
|||
cmip5 output1 MPI-M MPI-ESM-LR noVolc1985 (MXELv8) |
1986-1995 |
noVolc1985 (1.3 hindcast without volcanoes (1985)) - Version 3: Hindcast without volcanoes. Additional 10yr run for experiment 1.1 from 1985 without including the Agung, El Chichon and Pinatubo eruptions. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The noVolc1985 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELv8 |
|
cmip5 output2 MPI-M MPI-ESM-LR noVolc1985 (MXELv82) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR noVolc1985, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXELv82 |
|||
cmip5 output1 MPI-M MPI-ESM-LR noVolc1990 (MXELv9) |
1991-2000 |
noVolc1990 (1.3 hindcast without volcanoes (1990)) - Version 3: Hindcast without volcanoes. Additional 10yr run for experiment 1.1 from 1990 without including the Agung, El Chichon and Pinatubo eruptions. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The noVolc1990 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELv9 |
|
cmip5 output2 MPI-M MPI-ESM-LR noVolc1990 (MXELv92) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR noVolc1990, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXELv92 |
|||
cmip5 output1 MPI-M MPI-ESM-LR volcIn2010 (MXELvo) |
2006-2015 |
volcIn2010 (1.4 decadal prediction with 2010 volcano) - Version 3: Pinatubo-like eruption imposed. Repeat of the experiment 1.1 2005 forecast with an imposed $-1òüPinatuboòý eruption in 2010. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-LR model: The volcIn2010 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXELvo |
|
cmip5 output2 MPI-M MPI-ESM-LR volcIn2010 (MXELvo2) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-LR volcIn2010, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXELvo2 |
Model: MPI-ESM-MR#
Experiment Name |
Data Access |
Period |
Description |
Data Citation |
|---|---|---|---|---|
cmip5 output1 MPI-M MPI-ESM-MR decadals (MXMRDEC) |
1961-2020 |
decadalYYYY (10-year hindcast/prediction initialized in year YYYY) - Version 2: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2013): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The decadal experiments, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMRDEC |
|
cmip5 output1 MPI-M MPI-ESM-MR decadal1960 (MXMR60) |
1961-1970 |
decadal1960 (10-year hindcast/prediction initialized in year 1960) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The decadal1960 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMR60 |
|
cmip5 output2 MPI-M MPI-ESM-MR decadal1960 (MXMR602) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR decadal1960, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR602 |
|||
cmip5 output1 MPI-M MPI-ESM-MR decadal1965 (MXMR65) |
1966-1975 |
decadal1965 (10-year hindcast/prediction initialized in year 1965) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The decadal1965 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMR65 |
|
cmip5 output2 MPI-M MPI-ESM-MR decadal1965 (MXMR652) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR decadal1965, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR652 |
|||
cmip5 output1 MPI-M MPI-ESM-MR decadal1970 (MXMR70) |
1971-1980 |
decadal1970 (10-year hindcast/prediction initialized in year 1970) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The decadal1970 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMR70 |
|
cmip5 output2 MPI-M MPI-ESM-MR decadal1970 (MXMR702) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR decadal1970, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR702 |
|||
cmip5 output1 MPI-M MPI-ESM-MR decadal1975 (MXMR75) |
1976-1985 |
decadal1975 (10-year hindcast/prediction initialized in year 1975) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The decadal1975 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMR75 |
|
cmip5 output2 MPI-M MPI-ESM-MR decadal1975 (MXMR752) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR decadal1975, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR752 |
|||
cmip5 output1 MPI-M MPI-ESM-MR decadal1980 (MXMR80) |
1981-1990 |
decadal1980 (10-year hindcast/prediction initialized in year 1980) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The decadal1980 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMR80 |
|
cmip5 output2 MPI-M MPI-ESM-MR decadal1980 (MXMR802) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR decadal1980, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR802 |
|||
cmip5 output1 MPI-M MPI-ESM-MR decadal1985 (MXMR85) |
1986-1995 |
decadal1985 (10-year hindcast/prediction initialized in year 1985) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The decadal1985 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMR85 |
|
cmip5 output2 MPI-M MPI-ESM-MR decadal1985 (MXMR852) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR decadal1985, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR852 |
|||
cmip5 output1 MPI-M MPI-ESM-MR decadal1990 (MXMR90) |
1991-2000 |
decadal1990 (10-year hindcast/prediction initialized in year 1990) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The decadal1990 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMR90 |
|
cmip5 output2 MPI-M MPI-ESM-MR decadal1990 (MXMR902) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR decadal1990, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR902 |
|||
cmip5 output1 MPI-M MPI-ESM-MR decadal1995 (MXMR95) |
1996-2005 |
decadal1995 (10-year hindcast/prediction initialized in year 1995) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The decadal1995 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMR95 |
|
cmip5 output2 MPI-M MPI-ESM-MR decadal1995 (MXMR952) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR decadal1995, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR952 |
|||
cmip5 output1 MPI-M MPI-ESM-MR decadal2000 (MXMR00) |
2001-2010 |
decadal2000 (10-year hindcast/prediction initialized in year 2000) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The decadal2000 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMR00 |
|
cmip5 output2 MPI-M MPI-ESM-MR decadal2000 (MXMR002) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR decadal2000, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR002 |
|||
cmip5 output1 MPI-M MPI-ESM-MR decadal2001 (MXMR01) |
2002-2011 |
decadal2001 (10-year hindcast/prediction initialized in year 2001) - Version 2: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-MR decadal2001, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR01 |
|
cmip5 output2 MPI-M MPI-ESM-MR decadal2001 (MXMR012) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR decadal2001, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR012 |
|||
cmip5 output1 MPI-M MPI-ESM-MR decadal2002 (MXMR02) |
2003-2012 |
decadal2002 (10-year hindcast/prediction initialized in year 2002) - Version 2: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-MR decadal2002, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR02 |
|
cmip5 output2 MPI-M MPI-ESM-MR decadal2002 (MXMR022) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR decadal2002, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR022 |
|||
cmip5 output1 MPI-M MPI-ESM-MR decadal2003 (MXMR03) |
2004-2013 |
decadal2003 (10-year hindcast/prediction initialized in year 2003) - Version 2: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-MR decadal2003, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR03 |
|
cmip5 output2 MPI-M MPI-ESM-MR decadal2003 (MXMR032) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR decadal2003, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR032 |
|||
cmip5 output1 MPI-M MPI-ESM-MR decadal2004 (MXMR04) |
2005-2014 |
decadal2004 (10-year hindcast/prediction initialized in year 2004) - Version 2: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-MR decadal2004, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR04 |
|
cmip5 output2 MPI-M MPI-ESM-MR decadal2004 (MXMR042) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR decadal2004, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR042 |
|||
cmip5 output1 MPI-M MPI-ESM-MR decadal2005 (MXMR05) |
2006-2015 |
decadal2005 (10-year hindcast/prediction initialized in year 2005) - Version 3: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The decadal2005 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMR05 |
|
cmip5 output2 MPI-M MPI-ESM-MR decadal2005 (MXMR052) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR decadal2005, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR052 |
|||
cmip5 output1 MPI-M MPI-ESM-MR decadal2006 (MXMR06) |
2007-2016 |
decadal2006 (10-year hindcast/prediction initialized in year 2006) - Version 2: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-MR decadal2006, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR06 |
|
cmip5 output2 MPI-M MPI-ESM-MR decadal2006 (MXMR062) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR decadal2006, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR062 |
|||
cmip5 output1 MPI-M MPI-ESM-MR decadal2007 (MXMR07) |
2008-2017 |
decadal2007 (10-year hindcast/prediction initialized in year 2007) - Version 2: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-MR decadal2007, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR07 |
|
cmip5 output2 MPI-M MPI-ESM-MR decadal2007 (MXMR072) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR decadal2007, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR072 |
|||
cmip5 output1 MPI-M MPI-ESM-MR decadal2008 (MXMR08) |
2009-2018 |
decadal2008 (10-year hindcast/prediction initialized in year 2008) - Version 2: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-MR decadal2008, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR08 |
|
cmip5 output2 MPI-M MPI-ESM-MR decadal2008 (MXMR082) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR decadal2008, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR082 |
|||
cmip5 output1 MPI-M MPI-ESM-MR decadal2009 (MXMR09) |
2010-2019 |
decadal2009 (10-year hindcast/prediction initialized in year 2009) - Version 2: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): cmip5 output1 MPI-M MPI-ESM-MR decadal2009, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR09 |
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cmip5 output2 MPI-M MPI-ESM-MR decadal2009 (MXMR092) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR decadal2009, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR092 |
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cmip5 output1 MPI-M MPI-ESM-MR decadal2010 (MXMR10) |
2011-2020 |
decadal2010 (10-year hindcast/prediction initialized in year 2010) - Version 2: The atmospheric composition (and other conditions) should be prescribed as in the historical run (expt. 3.2) and the RCP4.5 scenario (expt. 4.1) of the long-term suite of experiments. Ocean initial conditions should be in some way representative of the observed anomalies or full fields for the start date. Land, sea-ice and atmosphere initial conditions are left to the discretion of each group. |
Jungclaus et al. (2012): CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on the MPI-ESM-MR model: The decadal2010 experiment, served by ESGF. WDCC at DKRZ. doi:10.1594/WDCC/CMIP5.MXMR10 |
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cmip5 output2 MPI-M MPI-ESM-MR decadal2010 (MXMR102) |
Jungclaus et al. (2014): cmip5 output2 MPI-M MPI-ESM-MR decadal2010, served by ESGF. WDCC at DKRZ. http://cera-www.dkrz.de/WDCC/CMIP5/Compact.jsp?acronym=MXMR102 |
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.
The near-term decadal prediction experiments are initialized from observed states of the climate system to explore climate predictability and prediction on decadal to multidecadal time scales. In these simulations, the models will not only respond, as in the long-term runs, to climate forcing (e.g., increasing atmospheric CO2 concentration) but also potentially track to some degree the actual trajectory of climate change, including (within the currently unknown predictability limits of the climate system) the unforced component of climate evolution. Note that decadal predictions with climate models are in an exploratory stage. A number of different methods are being tried to assimilate ocean observations into the models, and no single method has gained widespread acceptance. Moreover, the quality and completeness of ocean observations may be insufficient to realize but a fraction of the predictability inherent in the system. Thus, the forecast systems being assembled for CMIP5 are clearly not considered operational, nor will they necessarily provide more realistic simulations than the long-term simulations. Taylor, Karl E., Ronald J. Stouffer, Gerald A. Meehl (2012). An Overview of CMIP5 and the Experiment Design. Bull. Amer. Meteor. Soc., 93, 485-498. *`doi:10.1175/BAMS-D-11-00094.1 <http://dx.doi.org/10.1175/BAMS-D-11-00094.1>`__*.