.. _7da64e336971f8f37376ed62076d96fc_CMIP5_decadal_experiments: ====================================== CMIP5 near-term Experiments of MPI-M ====================================== **Results of long-term experiments are listed on a separate page:** :ref:`CMIP5 long-term Experiments of MPI-M <96b7b76346560c86d577a5ded2714b80_CMIP5_experiments>`.   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 `__\ *.*