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)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1960 (MXEL60)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1960 (MXEL602)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1961 (MXEL61)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1961 (MXEL612)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1962 (MXEL62)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1962 (MXEL622)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1963 (MXEL63)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1963 (MXEL632)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1964 (MXEL64)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1964 (MXEL642)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1965 (MXEL65)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1965 (MXEL652)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1966 (MXEL66)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1966 (MXEL662)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1967 (MXEL67)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1967 (MXEL672)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1968 (MXEL68)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1968 (MXEL682)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1969 (MXEL69)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1969 (MXEL692)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1970 (MXEL70)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1970 (MXEL702)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1971 (MXEL71)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1971 (MXEL712)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1972 (MXEL72)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1972 (MXEL722)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1973 (MXEL73)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1973 (MXEL732)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1974 (MXEL74)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1974 (MXEL742)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1975 (MXEL75)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1975 (MXEL752)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1976 (MXEL76)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1976 (MXEL762)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1977 (MXEL77)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1977 (MXEL772)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1978 (MXEL78)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1978 (MXEL782)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1979 (MXEL79)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1979 (MXEL792)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1980 (MXEL80)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1980 (MXEL802)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1981 (MXEL81)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1981 (MXEL812)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1982 (MXEL82)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1982 (MXEL822)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1983 (MXEL83)

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

cmip5 output2 MPI-M MPI-ESM-LR decadal1983 (MXEL832)

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

cmip5 output1 MPI-M MPI-ESM-LR decadal1984 (MXEL84)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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)

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

cmip5 output2 MPI-M MPI-ESM-MR decadal2009 (MXMR092)

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

cmip5 output1 MPI-M MPI-ESM-MR decadal2010 (MXMR10)

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

cmip5 output2 MPI-M MPI-ESM-MR decadal2010 (MXMR102)

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>`__*.