| Name | Triffid Movie | Isotope Movie | Description |
| GLAC_01 | Yes | n | This is a set of simulations using the latest version of HadCM3 with the latest Lev Tarasov GLAC ice sheet. Identical model setup to peltier_06/07 except using GLAC instead of Peltier.. More details of the simulations included in movie sequence can be found here |
| GLAC_02 | Yes | n | This is a set of simulations using the latest version of HadCM3 with the latest Lev Tarasov GLAC ice sheet. Identical model setup to peltier_06/07 except using GLAC instead of Peltier. This version has Russian rivers entering the Arctic.. More details of the simulations included in movie sequence can be found here |
| GLAC_02a | Yes | n | This is a set of simulations using the latest version of HadCM3 with the latest Lev Tarasov GLAC ice sheet. Identical model setup to peltier_06/07 except using GLAC instead of Peltier. This version has Russian rivers entering the Arctic.. More details of the simulations included in movie sequence can be found here |
| GLAC_03 | Yes | n | This is a set of simulations using the latest version of HadCM3 with the latest Lev Tarasov GLAC ice sheet. Identical model setup to peltier_06/07 except using GLAC instead of Peltier.. More details of the simulations included in movie sequence can be found here |
| GLAC_03a | Yes | n | This is a set of simulations using the latest version of HadCM3 with the latest Lev Tarasov GLAC ice sheet. Identical model setup to peltier_06/07 except using GLAC instead of Peltier.. More details of the simulations included in movie sequence can be found here |
| GLAC_04 | Yes | n | This is a set of simulations using the latest version of HadCM3 with the latest Lev Tarasov GLAC ice sheet. Identical model setup to peltier_06/07 except using GLAC instead of Peltier.. More details of the simulations included in movie sequence can be found here |
| GLAC_04a | Yes | n | This is a set of simulations using the latest version of HadCM3 with the latest Lev Tarasov GLAC ice sheet. Identical model setup to peltier_06/07 except using GLAC instead of Peltier.. More details of the simulations included in movie sequence can be found here |
| GLAC_05 | Yes | n | This is a set of simulations using the latest version of HadCM3 with the latest Lev Tarasov GLAC ice sheet. Identical model setup to peltier_06/07 except using GLAC instead of Peltier. Rivers draining to Med.. More details of the simulations included in movie sequence can be found here |
| GLAC_06 | Yes | n | This is a set of simulations using the latest version of HadCM3 with the latest Lev Tarasov GLAC ice sheet. Identical model setup to peltier_06/07 except using GLAC instead of Peltier. Rivers draining to Med.. More details of the simulations included in movie sequence can be found here |
| bbc_all_01 | n | n | This is a simulation using HadCM3 MOSESI for the last 120,000 years. The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. The simulations from 80kyr to 40kyr are very similar to those in bbc_original_01 but there are very small improvements in the ocean bathymetry i.e. they are a better reflection of the Peltier data. All simulations are 100 years long, initialised from a pre-industrial simulation.. More details of the simulations included in movie sequence can be found here |
| bbc_all_02 | n | n | This is a simulation using HadCM3 MOSESI for2 the last 120,000 years.2 the simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. The simulations from 80kyr to 40kyr are very similar to those in bbc_all_01 but there are very small improvements in the ocean bathymetry i.e. they are a better reflection of the Peltier data. All simulations are 200 years long, initialised from a pre-industrial simulation.. More details of the simulations included in movie sequence can be found here |
| bbc_all_03 | n | n | This is a simulation using HadCM3 MOSESI for the last 120,000 years.The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. The simulations from 80kyr to 40kyr are very similar to those in bbc_original_01 but there are very small improvements in the ocean bathymetry i.e. they are a better reflection of the Peltier data. All simulations are 500 years long, initialised from a pre-industrial simulation.. More details of the simulations included in movie sequence can be found here |
| bbc_all_03_Deglac | n | n | This is a simulation using HadCM3 MOSESI for the last 120,000 years.The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. The simulations from 80kyr to 40kyr are very similar to those in bbc_original_01 but there are very small improvements in the ocean bathymetry i.e. they are a better reflection of the Peltier data. All simulations are 500 years long, initialised from a pre-industrial simulation.. More details of the simulations included in movie sequence can be found here |
| bbc_all_03_Holocene | n | n | This is a simulation using HadCM3 MOSESI for the last 120,000 years.The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. The simulations from 80kyr to 40kyr are very similar to those in bbc_original_01 but there are very small improvements in the ocean bathymetry i.e. they are a better reflection of the Peltier data. All simulations are 500 years long, initialised from a pre-industrial simulation.. More details of the simulations included in movie sequence can be found here |
| bbc_all_04 | n | n | This differs from the bbc_all_03 set only in that full output is turned on so more detailed analysis of storm tracks etc can be undertaken. It is an extenstion of the runs for 100 years. Otherwise descrption below is the same as bbc_all_03. This is a simulation using HadCM3 MOSESI for the last 120,000 years.The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. The simulations from 80kyr to 40kyr are very similar to those in bbc_original_01 but there are very small improvements in the ocean bathymetry i.e. they are a better reflection of the Peltier data. All simulations are 600 years long, initialised from a pre-industrial simulation.. More details of the simulations included in movie sequence can be found here |
| bbc_all_iso_01 | Yes | y | This is a simulation using HadCM3 MOSES2 for the last 120,000 years including isotopes. It is a repeat of tdac series but with revised dark respiration term. The simulation uses snapshots every 4000 years from 120kyr to 80kyr, then every 2000 years to 22,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. This set of simulations uses the newer tctc series of ice sheets. This is part of several sets of simulations. This version is using dynamic TRIFFID and all forcings.. More details of the simulations included in movie sequence can be found here |
| bbc_all_isotopes_eqm_Holocene | Yes | y | This is a simulation using HadCM3 MOSES2 for the last 8,000 years with isotopes included. This is identical to the tdab series of experiments. This set of simulations uses the newer tctc series of ice sheets. This is part of several sets of simulations. This version is using dynamic TRIFFID and all forcings.. More details of the simulations included in movie sequence can be found here |
| bbc_all_triff_dyn | Yes | n | This is a simulation using HadCM3 MOSES2 for the last 120,000 years.The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. This set of simulations uses the newer tctc series of ice sheets. This is part of several sets of simulations. This version is using dynamic TRIFFID and all forcings.. More details of the simulations included in movie sequence can be found here |
| bbc_all_triff_dyn_Deglac | Yes | n | This is a simulation using HadCM3 MOSES2 for the last 120,000 years.The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. This set of simulations uses the newer tctc series of ice sheets. This is part of several sets of simulations. This version is using dynamic TRIFFID and all forcings.. More details of the simulations included in movie sequence can be found here |
| bbc_all_triff_dyn_Holocene | Yes | n | This is a simulation using HadCM3 MOSES2 for the last 120,000 years.The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. This set of simulations uses the newer tctc series of ice sheets. This is part of several sets of simulations. This version is using dynamic TRIFFID and all forcings.. More details of the simulations included in movie sequence can be found here |
| bbc_all_triff_eqm | Yes | n | This is a simulation using HadCM3 MOSES2 for the last 120,000 years.The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. This set of simulations uses the newer tctc series of ice sheets. This is part of several sets of simulations. This version is using equilibrium TRIFFID and all forcings.. More details of the simulations included in movie sequence can be found here |
| bbc_all_triff_fix | Yes | n | This is a simulation using HadCM3 MOSES2 for the last 120,000 years.The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. This set of simulations uses the newer tctc series of ice sheets. This is part of several sets of simulations. This version is using MOSES2.1 with fixed, prescribed pre-industrial vegetation and all forcings.. More details of the simulations included in movie sequence can be found here |
| bbc_all_triff_rev_dyn05 | Yes | n | This is a simulation using HadCM3 MOSES2.1 for the last 140,000 years. Using salinity correction update. Contination of teil for 1000 more years (5300 in total). It is a repeat of tdac series but with revised dark respiration term. The simulation uses snapshots every 2000 years from 130kyr to 80kyr, then every 2000 years to 22,000 years, and then every 1000 years from there until pre-industrial. There is one simulation fo 140kyr. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. This set of simulations uses the newer tctc series of ice sheets. This is part of several sets of simulations. This version is using dynamic TRIFFID and all forcings.. More details of the simulations included in movie sequence can be found here |
| bbc_all_triff_rev_dyn_Deglac | Yes | n | This is the last 21,000 years from a simulation using HadCM3 MOSES2.1 for the last 120,000 years. It is a repeat of tdac series but with revised dark respiration term. The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. This set of simulations uses the newer tctc series of ice sheets (based on Peltier 5G). This is part of several sets of simulations. This version is using dynamic TRIFFID and all forcings.. More details of the simulations included in movie sequence can be found here |
| bbc_all_triff_rev_dyn_extended | Yes | n | This is a simulation using HadCM3 MOSES2 for the last 130,000 years. It is a repeat of tdac series but with revised dark respiration term. The simulation uses snapshots every 2000 years from 120,000 years to 22,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. This set of simulations uses the newer tctc series of ice sheets. This is part of several sets of simulations. This version is using dynamic TRIFFID and all forcings.. More details of the simulations included in movie sequence can be found here |
| bbc_all_triff_rev_eqm | Yes | n | This is a simulation using HadCM3 MOSES2 for the last 120,000 years. It is a repeat of tdab series but with revised dark respiration term. The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. This set of simulations uses the newer tctc series of ice sheets. This is part of several sets of simulations. This version is using equilibrium TRIFFID and all forcings.. More details of the simulations included in movie sequence can be found here |
| bbc_all_triff_rev_sens | Yes | n | This is a simulation using HadCM3 MOSES2 for the last 120,000 years. It is an extension of the tdxo series (static veg) but with CO2 doubled in all runs to examine climate sensitivity. It uses the revised dark respiration term. The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. This set of simulations uses the newer tctc series of ice sheets. This is part of several sets of simulations. This version is using static vegetation in MOSES2 (pre-industrial from tdwza) and all forcings.. More details of the simulations included in movie sequence can be found here |
| bbc_all_triff_rev_sens4 | Yes | n | This is a simulation using HadCM3 MOSES2 for the last 120,000 years. It is an extension of the tdxo series (static veg) but with CO2 quadrupled in all runs to examine climate sensitivity. It uses the revised dark respiration term. The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. This set of simulations uses the newer tctc series of ice sheets. This is part of several sets of simulations. This version is using static vegetation in MOSES2 (pre-industrial from tdwza) and all forcings.. More details of the simulations included in movie sequence can be found here |
| bbc_all_triff_rev_stat | Yes | n | This is a simulation using HadCM3 MOSES2 for the last 120,000 years. It is a repeat of tdac series but with revised dark respiration term. The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. This set of simulations uses the newer tctc series of ice sheets. This is part of several sets of simulations. This version is using static vegetation in MOSES2 (pre-industrial from tdwza) and all forcings.. More details of the simulations included in movie sequence can be found here |
| bbc_easia_agcm_01 | n | n | This is a simulation of HadAM3 and was designed to provide lateral boundary condition files for the regional model similations (in bbc_easia_rcm_01. The simulation uses snapshots every 1000 years. The boundary conditions are the same as the bbcn_all_03 experiments (i.e. revised ice sheet based on Peltier Ice5G, and includes forcings from changes in ice sheet, land sea mask, greenhouses gases and orbits. The SST's and seaice come from the bbcn_all_03 simulations. The lateral boundary conditions are used to drive the regional model.. More details of the simulations included in movie sequence can be found here |
| bbc_easia_rcm_01 | n | n | This is a simulation using the E.Asian version of HadRM3 MOSESI for the last 21,000 years. The simulation uses snapshots every 1000 years. The boundary conditions are the same as the bbcn_all_03 experiments (i.e. revised ice sheet based on Peltier Ice5G, and includes forcings from changes in ice sheet, land sea mask, greenhouses gases and orbits. The SST's and seaice come from the bbcn_all_03 simulations. The lateral boundary conditions come from an equivalent run of the HadAM3 model with identical boundary conditions to above.. More details of the simulations included in movie sequence can be found here |
| bbc_eur_agcm_01 | n | n | This is a simulation of HadAM3 and was designed to provide lateral boundary condition files for the regional model similations (in bbc_eur_rcm_01. The simulation uses snapshots every 1000 years. The boundary conditions are the same as the bbcn_all_03 experiments (i.e. revised ice sheet based on Peltier Ice5G, and includes forcings from changes in ice sheet, land sea mask, greenhouses gases and orbits. The SST's and seaice come from the bbcn_all_03 simulations. The lateral boundary conditions are used to drive the regional model.. More details of the simulations included in movie sequence can be found here |
| bbc_eur_rcm_01 | n | n | This is a simulation using the European version of HadRM3 MOSESI for the last 21,000 years. The simulation uses snapshots every 1000 years. The boundary conditions are the same as the bbcn_all_03 experiments (i.e. revised ice sheet based on Peltier Ice5G, and includes forcings from changes in ice sheet, land sea mask, greenhouses gases and orbits. The SST's and seaice come from the bbcn_all_03 simulations. The lateral boundary conditions come from an equivalent run of the HadAM3 model with identical boundary conditions to above.. More details of the simulations included in movie sequence can be found here |
| bbc_hadam3h_Deglac | n | n | This is a set of simulations using HadAM3H MOSESI. They are driven from the bbcn_all SSTs and otherwise have the same boundary condtions as the latter runs.. More details of the simulations included in movie sequence can be found here |
| bbc_long_01 | Yes | n | WARNING: A bug was discovered in these runs, in which the ice sheet elevation changed but the ice sheet area did not. See bbc_long_03 for the corrected version. This is a simulation using HadCM3 MOSES2.1aD for the last 800,000 years. This uses the latest setup of HadCM3 (as of Jan 2019), and is the same as the teii series of bbc runs referred to as bbc_all_triff_rev_dyn04. It is forced with changing greenhouse gases, ice sheet from DeBoer et al 2013, and corresponding ocean salinity. Each simulation is 1000 years, initialised from the nearest equivalent (based on sea level) simulation from the teii series. Simulations are every 4kyr from 800kyr to 24kyr, after which they are 1kyr BP intervals.. More details of the simulations included in movie sequence can be found here |
| bbc_long_02 | Yes | n | WARNING: A bug was discovered in these runs, in which the ice sheet elevation changed but the ice sheet area did not. See bbc_long_03 for the corrected version. This is as bbc_long_01 but produces more extensive output. All of the simulations were started from the end of the corresponding bbc_long_01 simulations, and continued for 150 years to capture the extended output. Otherwise identical to bbc_long_01, ie.. simulations using HadCM3 MOSES2.1aD for the last 800,000 years. This uses the latest setup of HadCM3 (as of Jan 2019), and is the same as the teii series of bbc runs referred to as bbc_all_triff_rev_dyn04. It is forced with changing greenhouse gases, ice sheet from DeBoer et al 2013, and corresponding ocean salinity. Each simulation is 150 years, initialised from the bbc_long_01 simulations. Simulations are every 4kyr from 800kyr to 24kyr, after which they are 1kyr BP intervals.. More details of the simulations included in movie sequence can be found here |
| bbc_long_03 | Yes | n | This is a corrected version of bbc_long_02. The ice sheet cover and the ice sheet elevation are correctly represented. This setup includes extensive output. Otherwise same as bbc_long01/02, namely this is a simulation using HadCM3 MOSES2.1aD for the last 800,000 years. This uses the latest setup of HadCM3 (as of Jan 2019), and is the same as the teii series of bbc runs referred to as bbc_all_triff_rev_dyn04. It is forced with changing greenhouse gases, ice sheet from DeBoer et al 2013, and corresponding ocean salinity. Each simulation is 500 years, initialised from the nearest equivalent (based on sea level) simulation from the teii series. Simulations are every 4kyr from 800kyr to 24kyr, after which they are 1kyr BP intervals.. More details of the simulations included in movie sequence can be found here |
| bbc_long_04 | Yes | n | As bbc_long_03 (corrected ice version) but using the latest version with improvements to atmospheric convection and land surface which improves the simulation of the N. African monsoon system (and also the East Asian monsoon). The simulation is using HadCM3BB MOSES2.1aD for the last 800,000 years. This uses the latest setup of HadCM3BB (as of May 2022), including a number of small bug fixes etc. It is forced with changing greenhouse gases, ice sheet from DeBoer et al 2013, and corresponding ocean salinity. Each simulation is 500 years, initialised from the bbc_long_03 simulations. Simulations are every 4kyr from 800kyr to 24kyr, after which they are 1kyr BP intervals. Extensive output.. More details of the simulations included in movie sequence can be found here |
| bbc_long_04a | Yes | n | This is a simulation using HadCM3 MOSES2.1aD for the last 800,000 years. This uses the latest setup of HadCM3 (as of May 2022), and is the same as the teii series of bbc runs referred to as bbc_all_triff_rev_dyn04. It is forced with changing greenhouse gases, ice sheet from DeBoer et al 2013, and corresponding ocean salinity. These are the first 100 years when the Sahara was held green. More details of the simulations included in movie sequence can be found here |
| bbc_long_05 | Yes | n | As bbc_long_04 (HadCM3BB) but with no changes to ice sheet. Hence changes to orbit and CO2 only. Using the latest version with improvements to atmospheric convection and land surface which improves the simulation of the N. African monsoon system (and also the East Asian monsoon). The simulation is using HadCM3BB MOSES2.1aD for the last 800,000 years. This uses the latest setup of HadCM3BB (as of May 2022), including a number of small bug fixes etc. It is forced with changing greenhouse gases, ice sheet from DeBoer et al 2013, and corresponding ocean salinity. Each simulation is 500 years, initialised from the bbc_long_04 simulations. Simulations are every 4kyr from 800kyr to 24kyr, after which they are 1kyr BP intervals. Extensive output.. More details of the simulations included in movie sequence can be found here |
| bbc_long_06 | Yes | n | As bbc_long_04 and 05 (HadCM3BB) but with no changes to ice sheet or CO2. Hence changes to orbit only. Using the latest version with improvements to atmospheric convection and land surface which improves the simulation of the N. African monsoon system (and also the East Asian monsoon). The simulation is using HadCM3BB MOSES2.1aD for the last 800,000 years. This uses the latest setup of HadCM3BB (as of May 2022), including a number of small bug fixes etc. It is forced with changing greenhouse gases, ice sheet from DeBoer et al 2013, and corresponding ocean salinity. Each simulation is 500 years, initialised from the bbc_long_04 simulations. Simulations are every 4kyr from 800kyr to 24kyr, after which they are 1kyr BP intervals. Extensive output.. More details of the simulations included in movie sequence can be found here |
| bbc_long_07 | Yes | n | As bbc_long_04 but extended to 3.6 million years. It is using the latest version with improvements to atmospheric convection and land surface which improves the simulation of the N. African monsoon system (and also the East Asian monsoon). It uses the latest setup of HadCM3BB (as of May 2022), including a number of small bug fixes etc. It is forced with changing greenhouse gases, ice sheet from DeBoer et al 2013, and corresponding ocean salinity. Each simulation is 500 years, initialised from the nearest bbc_long_04 simulations. Simulations are every 4kyr from 800kyr to 24kyr, after which they are 1kyr BP intervals. Extensive output.. More details of the simulations included in movie sequence can be found here |
| bbc_long_08 | Yes | n | As bbc_long_04 but extended for a further 500 years with the corrected orbital bug. Also using an updated orbit (Laskar, 2010). All other details the same as bbc_long_04 (i.e. orbit, RAGS and ice sheet/land mask changing.. More details of the simulations included in movie sequence can be found here |
| bbc_long_09 | Yes | n | As bbc_long_05 (i.e. no ice sheet change, but changes in orbit and CO2) but extended for a further 500 years with the corrected orbital bug. Also using an updated orbit (Laskar, 2010). All other details the same as bbc_long_04 (i.e. orbit, RAGS).. More details of the simulations included in movie sequence can be found here |
| bbc_long_10 | Yes | n | As bbc_long_06 (i.e. only changing orbit) but extended for a further 500 years with the corrected orbital bug. Also using an updated orbit (Laskar, 2010). All other details the same as bbc_long_04 (i.e. orbit only).. More details of the simulations included in movie sequence can be found here |
| bbc_long_11 | Yes | n | As bbc_long_07 but corrected orbit calculation, extended to 3.6 million years. It is using the latest version with improvements to atmospheric convection and land surface which improves the simulation of the N. African monsoon system (and also the East Asian monsoon). It uses the latest setup of HadCM3BB (as of May 2022), including a number of small bug fixes etc. It is forced with changing greenhouse gases, ice sheet from DeBoer et al 2013, and corresponding ocean salinity. Each simulation is 500 years, initialised from the nearest bbc_long_04 simulations. Simulations are every 4kyr from 3600kyr to 24kyr, after which they are 1kyr BP intervals. Extensive output.. More details of the simulations included in movie sequence can be found here |
| bbc_long_12 | Yes | n | As bbc_long_11 (corrected 3.6Ma bbc_long) but with no ice sheets changing (but orbit and GHGs). It is using the latest version with improvements to atmospheric convection and land surface which improves the simulation of the N. African monsoon system (and also the East Asian monsoon). It uses the latest setup of HadCM3BB (as of May 2022), including a number of small bug fixes etc. It is forced with changing greenhouse gases, ice sheet from DeBoer et al 2013, and corresponding ocean salinity. Each simulation is 500 years, initialised from the nearest bbc_long_04 simulations. Simulations are every 4kyr from 3600kyr to 24kyr, after which they are 1kyr BP intervals. Extensive output.. More details of the simulations included in movie sequence can be found here |
| bbc_long_13 | Yes | n | As bbc_long_11 (corrected 3.6Ma bbc_long) but with no ice sheets or GHGs changing (only orbit). It is using the latest version with improvements to atmospheric convection and land surface which improves the simulation of the N. African monsoon system (and also the East Asian monsoon). It uses the latest setup of HadCM3BB (as of May 2022), including a number of small bug fixes etc. It is forced with changing greenhouse gases, ice sheet from DeBoer et al 2013, and corresponding ocean salinity. Each simulation is 500 years, initialised from the nearest bbc_long_04 simulations. Simulations are every 4kyr from 3600kyr to 24kyr, after which they are 1kyr BP intervals. Extensive output.. More details of the simulations included in movie sequence can be found here |
| bbc_long_14 | Yes | n | As bbc_long_11 (corrected 3.6Ma bbc_long) but with ice sheets and orbit changing but not GHGs). It is using the latest version with improvements to atmospheric convection and land surface which improves the simulation of the N. African monsoon system (and also the East Asian monsoon). It uses the latest setup of HadCM3BB (as of May 2022), including a number of small bug fixes etc. It is forced with changing greenhouse gases, ice sheet from DeBoer et al 2013, and corresponding ocean salinity. Each simulation is 500 years, initialised from the nearest bbc_long_04 simulations. Simulations are every 4kyr from 3600kyr to 24kyr, after which they are 1kyr BP intervals. Extensive output.. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_01 | n | n | This is a simulation using HadCM3 MOSESI for the last 120,000 years. The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing includs changing orbits only. All simulations are 100 years long, initialised from a pre-industrial simulation.. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_01a | n | n | This is a simulation using HadCM3 MOSESI for the last 120,000 years. The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing includs changing orbits only. All simulations are 100 years long, initialised from a pre-industrial simulation.. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_02 | n | n | This is a simulation using HadCM3 MOSESI for the last 120,000 years. The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing includs changing orbits only. All simulations are 200 years long, initialised from a pre-industrial simulation.. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_02a | n | n | This is a simulation using HadCM3 MOSESI for the last 120,000 years. The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing includs changing orbits only. All simulations are 200 years long, initialised from a pre-industrial simulation.. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_03 | n | n | This is a simulation using HadCM3 MOSESI for the last 120,000 years. The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing includs changing orbits only. All simulations are 500 years long, initialised from a pre-industrial simulation.. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_03a | n | n | This is a simulation using HadCM3 MOSESI for the last 120,000 years. The simulation uses snapshots every 2000 or 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing includs changing orbits only. All simulations are 500 years long, initialised from a pre-industrial simulation.. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_GHG_01 | n | n | This is a simulation using HadCM3 MOSESI for the last 140,000 years. The simulation uses snapshots every 2000 years from 140,000 years to 120,000 years, then 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changing orbits and trace gases. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_GHG_01a | n | n | This is a simulation using HadCM3 MOSESI for the last 140,000 years. The simulation uses snapshots every 2000 years from 140,000 years to 120,000 years, then 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changing orbits and trace gases. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_GHG_02 | n | n | This is a simulation using HadCM3 MOSESI for the last 140,000 years. The simulation uses snapshots every 2000 years from 140,000 years to 120,000 years, then 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changing orbits and trace gases. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_GHG_02a | n | n | This is a simulation using HadCM3 MOSESI for the last 140,000 years. The simulation uses snapshots every 2000 years from 140,000 years to 120,000 years, then 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changing orbits and trace gases. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_GHG_03 | n | n | This is a simulation using HadCM3 MOSESI for the last 140,000 years. The simulation uses snapshots every 2000 years from 140,000 years to 120,000 years, then 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changing orbits and trace gases. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_GHG_03a | n | n | This is a simulation using HadCM3 MOSESI for the last 140,000 years. The simulation uses snapshots every 2000 years from 140,000 years to 120,000 years, then 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changing orbits and trace gases. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_GHG_ice_01 | n | n | This is a simulation using HadCM3 MOSESI for the last 80,000 to 40,000 years. Forcing is with changed icesheets, changing orbits and trace gases, but no change of land sea mask. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_GHG_interglacial | Yes | n | This is a set of simulations using HadCM3 MOSES1 for previous interglacials. The version of the model is identical to that of bbc_all_03. There is no changes in land or ice masks, purely orbit and greenhouse gases.. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_GHG_triff_dyn | Yes | n | This is a simulation using HadCM3 MOSES2 for the last 120,000 years.The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changing orbits and trace gases. This set of simulations uses the newer tctc series of ice sheets. This is part of several sets of simulations. This version is using dynamic TRIFFID and orbit+GHG forcings.. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_GHG_triff_eqm | Yes | n | This is a simulation using HadCM3 MOSES2 for the last 120,000 years.The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changing orbits and trace gases. This set of simulations uses the newer tctc series of ice sheets. This is part of several sets of simulations. This version is using equilibrium TRIFFID and orbit+GHG forcings.. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_GHG_triff_rev_dyn | Yes | n | This is a simulation using HadCM3 MOSES2 for the last 120,000 years. It is a repeat of tdac series but with revised dark respiration term. The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. This set of simulations uses the newer tctc series of ice sheets. This is part of several sets of simulations. This version is using dynamic TRIFFID and all forcings. This had a mistake so that all orbits are for 1kyr BP except for the pre-industrial itself.. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_GHG_triff_rev_sens | Yes | n | This is a simulation using HadCM3 MOSES2 for the last 120,000 years. It is an extension of the tdxo series (static veg) but with CO2 doubled in all runs to examine climate sensitivity. It uses the revised dark respiration term. The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. This set of simulations uses the newer tctc series of ice sheets. This is part of several sets of simulations. This version is using static vegetation in MOSES2 (pre-industrial from tdwza) and all forcings. This had a mistake so that all orbits are for 1kyr BP except for the pre-industrial itself.. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_GHG_triff_rev_stat | Yes | n | This is a simulation using HadCM3 MOSES2 for the last 120,000 years. It is a repeat of tdac series but with revised dark respiration term. The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. This set of simulations uses the newer tctc series of ice sheets. This is part of several sets of simulations. This version is using static vegetation in MOSES2 (pre-industrial from tdwza) and all forcings. It had a mistake so that all orbits are for 1kyr BP except for the pre-industrial itself.. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_triff_dyn | Yes | n | This is a simulation using HadCM3 MOSES2 for the last 120,000 years.The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changing orbits only. This set of simulations uses the newer tctc series of ice sheets. This is part of several sets of simulations. This version is using dynamic TRIFFID and orbital forcing only.. More details of the simulations included in movie sequence can be found here |
| bbc_orbit_triff_eqm | Yes | n | This is a simulation using HadCM3 MOSES2 for the last 120,000 years.The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changing orbits only. This set of simulations uses the newer tctc series of ice sheets. This is part of several sets of simulations. This version is using equilibrium TRIFFID and orbital forcing only.. More details of the simulations included in movie sequence can be found here |
| bbc_original_01 | n | n | This is a simulation using HadCM3 MOSESI from 80,000 to 40,000 years. The simulation uses snapshots every 4000 years (more frequent for the last 21,000 years). Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. More details of the simulations included in movie sequence can be found here |
| bbcn_all_03 | n | n | This sequence of simulations is a new version of the BBC runs using a revised, improved ice sheet over the original BBC runs. In the latter part of the sequence the improvements were related to better including isostatic adjustment. This isusing HadCM3 MOSESI for the last 120,000 years.The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. The simulations from 80kyr to 40kyr are very similar to those in bbc_original_01 but there are very small improvements in the ocean bathymetry i.e. they are a better reflection of the Peltier data. All simulations are 500 years long, initialised from a pre-industrial simulation.. More details of the simulations included in movie sequence can be found here |
| bbcn_all_03_Deglac | n | n | This sequence of simulations is a new version of the BBC runs using a revised, improved ice sheet over the original BBC runs. In the latter part of the sequence the improvements were related to better including isostatic adjustment. This isusing HadCM3 MOSESI for the last 120,000 years.The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. The simulations from 80kyr to 40kyr are very similar to those in bbc_original_01 but there are very small improvements in the ocean bathymetry i.e. they are a better reflection of the Peltier data. All simulations are 500 years long, initialised from a pre-industrial simulation.. More details of the simulations included in movie sequence can be found here |
| bbcn_all_03_Holocene | n | n | This sequence of simulations is a new version of the BBC runs using a revised, improved ice sheet over the original BBC runs. In the latter part of the sequence the improvements were related to better including isostatic adjustment. This isusing HadCM3 MOSESI for the last 120,000 years.The simulation uses snapshots every 4000 years for the time period from 120,000 years to 80,000 years, then every 2000 years from 80,000 years to 21,000 years, and then every 1000 years from there until pre-industrial. Forcing is with changed icesheets, changing orbits and trace gases, and land sea mask. The simulations from 80kyr to 40kyr are very similar to those in bbc_original_01 but there are very small improvements in the ocean bathymetry i.e. they are a better reflection of the Peltier data. All simulations are 500 years long, initialised from a pre-industrial simulation.. More details of the simulations included in movie sequence can be found here |
| bham_holocene_conv | n | n | 500 year spaced snapshots from a 10,000 year transient Holocene simulation run on BEAR at U of Birmingham. Branched from Peltier6g deglaciation run 07. This model configuration employs changes to the entrainment rate and convection scheme that causes a much stronger monsoon response to mid-Holocene boundary conditions.. More details of the simulations included in movie sequence can be found here |
| bham_holocene_solar_vmsconv | n | n | 500 year spaced snapshots from a 10,000 year transient Holocene simulation run on BEAR at U of Birmingham. Branched from Peltier6g deglaciation run 07. This model configuration combines the vegetatoin and convection changes. Includes transient solar forcing over the Holocene.. More details of the simulations included in movie sequence can be found here |
| bham_holocene_solarvolc_vmsconv | n | n | 500 year spaced snapshots from a 10,000 year transient Holocene simulation run on BEAR at U of Birmingham. Branched from Peltier6g deglaciation run 07. This model configuration combines the vegetatoin and convection changes. Includes transient solar and volcanic forcing over the Holocene. More details of the simulations included in movie sequence can be found here |
| bham_holocene_std | n | n | 500 year spaced snapshots from a 10,000 year transient Holocene simulation run on BEAR at U of Birmingham. Branched from Peltier6g deglaciation run 07.. More details of the simulations included in movie sequence can be found here |
| bham_holocene_vms | n | n | 500 year spaced snapshots from a 10,000 year transient Holocene simulation run on BEAR at U of Birmingham. Branched from Peltier6g deglaciation run 07. This model version has an optimised moisture stress for vegetation that favour vegetation in semi-arid regions.. More details of the simulations included in movie sequence can be found here |
| bham_holocene_vmsconv | n | n | 500 year spaced snapshots from a 10,000 year transient Holocene simulation run on BEAR at U of Birmingham. Branched from Peltier6g deglaciation run 07. This model configuration combines the vegetatoin and convection changes.. More details of the simulations included in movie sequence can be found here |
| famous_02_deglac | n | n | This is a simulation using FAMOUS for the last 21,000 years. These simulations are fully time continuous and you can get every month of the run but the climate means correspond to the end of each 1000 year section.. More details of the simulations included in movie sequence can be found here |
| famous_deglac_acc_01 | n | n | Famous deglaciation run (20k-9k), where land-sea mask and ice-sheet sizes are the only changes. Orbital forcing and ghg are fixed at 21k level. accelerated run (X10). More details of the simulations included in movie sequence can be found here |
| famous_deglac_acc_02 | n | n | Famous deglaciation run (21k-9k). Land-sea mask, ice-sheet sizes, orbital forcing and ghg are changing through the run. accelerated run (X10). More details of the simulations included in movie sequence can be found here |
| famous_orbit_01 | n | n | This is the first (idealised) simulation of FAMOUS for the last 21,000 years. The simulation uses acceleration (10x) and includes just changing orbits only.. More details of the simulations included in movie sequence can be found here |
| famous_orbit_GHG_01 | n | n | This is a simulation of FAMOUS for the last 21,000 years. The simulation uses acceleration (10x) and includes just changing orbits and trace gas changes. More details of the simulations included in movie sequence can be found here |
| getech_01 | n | n | This is Phase 3 GETECH showing sequence through Cretaceous. More details of the simulations included in movie sequence can be found here |
| getech_02 | n | n | This is Phase 4 GETECH showing sequence through Cretaceous (at 4xCO2). More details of the simulations included in movie sequence can be found here |
| getech_03 | n | n | This is Phase 3 GETECH showing sequence through Cretaceous and Cenozoic. More details of the simulations included in movie sequence can be found here |
| getech_04 | Yes | n | This is Phase 4 GETECH showing sequence through Cretaceous and Cenozoic. More details of the simulations included in movie sequence can be found here |
| getech_05a | Yes | n | This is the end of the long 5000 year spinups of GETECH showing sequence through Cretaceous and part of Cenozoic using 4xCO2. More details of the simulations included in movie sequence can be found here |
| getech_05b | Yes | n | This is the end of the long 5000 year spinups of GETECH showing sequence through Cretaceous and part of Cenozoic using 2xCO2. More details of the simulations included in movie sequence can be found here |
| getech_06 | Yes | n | This is Phase 4 GETECH showing sequence through the Permian, Mesozoic, and Cenozoic. More details of the simulations included in movie sequence can be found here |
| getech_06a | Yes | n | This is Phase 4 GETECH showing sequence through the Cenozoic only. More details of the simulations included in movie sequence can be found here |
| getech_07 | Yes | n | This is Phase 6 GETECH showing sequence through the Cenozoic. This is old cloud physics.. More details of the simulations included in movie sequence can be found here |
| getech_08 | Yes | n | This is Phase 7 GETECH showing sequence through the Cenozoic. This is new cloud physics.. More details of the simulations included in movie sequence can be found here |
| getech_09 | Yes | n | This is Phase 8 GETECH showing sequence through the Cenozoic. This is new cloud physics and realistic CO2.. More details of the simulations included in movie sequence can be found here |
| holo_land_01 | n | n | This is set of simulations using HadCM3 MOSES2.1 dynamic vegetation for the last 8000 years with land use included. This particular version uses the HYDE reconstructions. The simulation uses snapshots every 1000 years. All simulations are 1000 years long, initialised from a pre-industrial simulation.. More details of the simulations included in movie sequence can be found here |
| holo_land_02 | n | n | This is set of simulations using HadCM3 MOSES2.1 dynamic vegetation for the last 8000 years. This particular version uses the KAPLAN reconstructions. The simulation uses snapshots every 1000 years. All simulations are 1000 years long, initialised from a pre-industrial simulation.. More details of the simulations included in movie sequence can be found here |
| holo_land_ctl | n | n | This is set of simulations using HadCM3 MOSES2.1 dynamic vegetation for the last 8000 years. This forms the control run for the Holocene land-use simulations. The simulation uses snapshots every 1000 years. All simulations are 1000 years long, initialised from a pre-industrial simulation.. More details of the simulations included in movie sequence can be found here |
| igs_orbit_GHG_03 | n | n | This is a simulation using HadCM3 MOSESI for the last 610,000 years. The simulation uses snapshots every 10, 5, or 4kyr. Forcing is with changing orbits and trace gases only.. More details of the simulations included in movie sequence can be found here |
| peltier_01 | n | n | This is a set of simulations using the latest version of HadCM3 with the latest Peltier 6GC ice sheet. Other boundary conditions are fairly standard.. More details of the simulations included in movie sequence can be found here |
| peltier_03 | n | n | This is a set of simulations using the latest version of HadCM3 with the latest Peltier 6GC ice sheet. Other boundary conditions are fairly standard.. More details of the simulations included in movie sequence can be found here |
| peltier_04 | n | n | This is a set of simulations using the latest version of HadCM3 with the latest Peltier 6GC ice sheet. Other boundary conditions are fairly standard. It is a continuation of peltier_03 set of simulations except that the salinity drift update has been removed (and the waterfix input has been adjusted accordingly). Also ensured that atmospheric mass was conserved.. More details of the simulations included in movie sequence can be found here |
| peltier_05 | n | n | This is a set of simulations using the latest version of HadCM3 with the latest Peltier 6GC ice sheet. Other boundary conditions are fairly standard. It is a continuation of peltier_04 set of simulations but with enhanced output for storm track and other analysis.. More details of the simulations included in movie sequence can be found here |
| peltier_06 | n | n | This is a set of simulations using the latest version of HadCM3 with the latest Peltier 6GC ice sheet. Very similar to peltier_03 but updated STASH, , solar constant, CO2 etc, salinity target, and most importantly, runoff maps. These are draft version of the final set for the transient runs. This version has Russian rivers entering the Med for the height of the glacial... More details of the simulations included in movie sequence can be found here |
| peltier_07 | n | n | This is a set of simulations using the latest version of HadCM3 with the latest Peltier 6GC ice sheet. Very similar to peltier_06 but this version has Russian rivers entering the Arctic throughout the deglaciation... More details of the simulations included in movie sequence can be found here |
| peltier_08g | Yes | n | This is a set of transient simulations using the latest version of HadCM3 with the latest Peltier 6GC ice sheet.. More details of the simulations included in movie sequence can be found here |
| peltier_08h | Yes | n | This is a set of transient simulations using the latest version of HadCM3 with the latest Peltier 6GC ice sheet.. More details of the simulations included in movie sequence can be found here |
| peltier_08i | Yes | n | This is a set of transient simulations using the latest version of HadCM3 with the latest Peltier 6GC ice sheet.. More details of the simulations included in movie sequence can be found here |
| peltier_08j | Yes | n | This is a set of transient simulations using the latest version of HadCM3 with the latest Peltier 6GC ice sheet.. More details of the simulations included in movie sequence can be found here |
| peltier_09 | n | n | This is a set of simulations using the latest version of HadCM3 with the latest Peltier 6GC ice sheet. Very similar to peltier_06 but updated CO2 etc so that they gases ar the same as the fully transient simulations. This set is the first 300 years of a 500 year run (peltier_09 is the final 200 years and has a very comprehensive STASH). This version has Russian rivers entering the Med for the height of the glacial... More details of the simulations included in movie sequence can be found here |
| peltier_09a | n | n | This is a set of simulations using the latest version of HadCM3 with the latest Peltier 6GC ice sheet. Very similar to peltier_06 but updated CO2 etc so that they gases ar the same as the fully transient simulations. This set is the first 300 years of a 500 year run (peltier_09 is the final 200 years and has a very comprehensive STASH). This version has Russian rivers entering the Med for the height of the glacial... More details of the simulations included in movie sequence can be found here |
| peltier_10 | n | n | This is a set of simulations using the latest version of HadCM3 with the latest Peltier 6GC ice sheet. Very similar to peltier_06 but updated CO2 etc so that they gases ar the same as the fully transient simulations. This set is the first 300 years of a 500 year run (peltier_09 is the final 200 years and has a very comprehensive STASH). This version has Russian rivers entering the Med for the height of the glacial... More details of the simulations included in movie sequence can be found here |
| peltier_10a | n | n | This is a set of simulations using the latest version of HadCM3 with the latest Peltier 6GC ice sheet. Very similar to peltier_06 but updated CO2 etc so that they gases ar the same as the fully transient simulations. This set is the first 300 years of a 500 year run (peltier_09 is the final 200 years and has a very comprehensive STASH). This version has Russian rivers entering the Med for the height of the glacial... More details of the simulations included in movie sequence can be found here |
| peltier_11 | n | n | This is a set of simulations using the latest version of HadCM3 with the latest Peltier 6GC ice sheet. This is using the bug fixed version of the orbit code, and the latest (as of late 2024) updates to the main code. This version has Russian rivers entering the Med for the height of the glacial... More details of the simulations included in movie sequence can be found here |
| peltier_latest | n | n | This is a set of simulations using the latest version of HadCM3 with the latest Peltier 6GC ice sheet. Very similar to peltier_06 but updated CO2 etc so that they gases ar the same as the fully transient simulations. This set is the first 300 years of a 500 year run (peltier_09 is the final 200 years and has a very comprehensive STASH). This version has Russian rivers entering the Med for the height of the glacial... More details of the simulations included in movie sequence can be found here |
| phan_01 | n | n | Similar to quaternary_01 but showing the changes in climate during the Phanerozoic (last 570 million years). More details of the simulations included in movie sequence can be found here |
| quaternary_01 | n | n | Produces output for the change in climate from 21k to pre-industrial, normally presented as a difference plot. More details of the simulations included in movie sequence can be found here |
| quaternary_01a | n | n | As quaternary_01 but better vertical resolution in the saved output variables (but model itself is the same). More details of the simulations included in movie sequence can be found here |
| quaternary_02 | n | n | Shows output every 3000 years for simulations which include vegetation feedback.. More details of the simulations included in movie sequence can be found here |
| roberts_01 | Yes | n | This is Robertsons Merlin+. Asselian, Toarcian, Kimmeridigian, Aptian, Turonian, Ypresian. More details of the simulations included in movie sequence can be found here |
| roberts_02 | Yes | n | This is Combination of Robertsons and GETECH showing sequence through Cretaceous and Cenozoic. More details of the simulations included in movie sequence can be found here |
| roberts_03 | Yes | n | This is Combination of Robertsons and GETECH showing sequence through Cretaceous and Cenozoic. More details of the simulations included in movie sequence can be found here |
| robertson_01 | Yes | n | This is new Robertsons sequence through Cretaceous and Cenozoic. More details of the simulations included in movie sequence can be found here |
| robertson_01a | Yes | n | This is new Robertsons sequence through Cretaceous and Cenozoic. More details of the simulations included in movie sequence can be found here |
| robertson_01all | Yes | n | This is new Robertsons sequence through Cretaceous and Cenozoic. More details of the simulations included in movie sequence can be found here |
| robertson_02 | Yes | n | This is new Robertsons sequence through Cretaceous and Cenozoic. More details of the simulations included in movie sequence can be found here |
| robertson_02all | Yes | n | This is new Robertsons sequence through Cretaceous and Cenozoic. More details of the simulations included in movie sequence can be found here |
| robertson_03 | Yes | n | This is new Robertsons sequence through Phanerozoic. More details of the simulations included in movie sequence can be found here |
| robertson_04 | Yes | n | This is new Robertsons sequence through Phanerozoic. More details of the simulations included in movie sequence can be found here |
| scotese_01 | Yes | n | This is the full results after the spinup simulations using Scotese palaeogeogs covering the whole of the Phanerozoic. More details of the simulations included in movie sequence can be found here |
| scotese_02 | Yes | n | This is as scotese_01 but with CO2 from Foster et al 2017.. More details of the simulations included in movie sequence can be found here |
| scotese_02_Cenozoic | Yes | n | This is using Chris Scotese paleogeogs but with CO2 from Foster et al 2017.. More details of the simulations included in movie sequence can be found here |
| scotese_02_original | Yes | n | This is as scotese_01 but with CO2 from Foster et al 2017. This was an early release with all model simulations run for 2000 years. Subsequently run for longer to become the definitive version.. More details of the simulations included in movie sequence can be found here |
| scotese_03 | Yes | n | This is as scotese_02 but revised model (cloud physics not no desert update). More details of the simulations included in movie sequence can be found here |
| scotese_03a | Yes | n | This is as scotese_02 but revised model (cloud physics not no desert update). More details of the simulations included in movie sequence can be found here |
| scotese_04 | Yes | n | This is as scotese_02 but revised model (cloud physics not no desert update) and updated ocean diffusion.. More details of the simulations included in movie sequence can be found here |
| scotese_05 | Yes | n | This is as scotese_04 but revised model (cloud physics) and updated ocean diffusion.. More details of the simulations included in movie sequence can be found here |
| scotese_06 | Yes | n | This is the latest scotese with islands and revised physics and Foster CO2. More details of the simulations included in movie sequence can be found here |
| scotese_07 | Yes | n | This is the latest scotese with islands and updated Rae et al CO2.. More details of the simulations included in movie sequence can be found here |
| scotese_08 | Yes | n | This is the latest scotese with islands and CO2 tuned for global mean temperature. It is identical to scotese_08a but this set of runs were for 3000 years BUT did not output all variables. scotese_08a represents an extension of these simulations (only for 110 years) but with a more comprehensive set of output.. More details of the simulations included in movie sequence can be found here |
| scotese_08a | Yes | n | This is the latest scotese with islands and CO2 tuned for global mean temperature. The simulations are relatively short (110 years) extensions of the tfks series which were all spun-up for 3000 years. If you need to look at spinup, use the scotese_08 set.. More details of the simulations included in movie sequence can be found here |
| scotese_2co2a | Yes | n | This is as scotese_solara but with 2x pre-industrial CO2. Initialised from the end of scotese_solara. These runs are 2000 years long.. More details of the simulations included in movie sequence can be found here |
| scotese_4co2a | Yes | n | This is as scotese_solara but with 4x pre-industrial CO2. Initialised from the end of scotese_solara. These runs are 2000 years long.. More details of the simulations included in movie sequence can be found here |
| scotese_OBC_01 | Yes | n | This is the latest Scotese with islands and Foster CO2, and using the latest ocean biogeochemistry code. They were started from the scotese_06a set (co2 tuned to Scotese temperatures) and extended because the initial set of simulations did not change the pCO2 of the ocean. It remained constant at 280ppm whereas.. More details of the simulations included in movie sequence can be found here |
| scotese_OBC_02 | Yes | n | This is the latest Scotese with islands and Foster CO2, and using the final ocean biogeochemistry code for HadCM3L. They were started from the scotese_OBG_01 set (co2 tuned to Scotese temperatures).. More details of the simulations included in movie sequence can be found here |
| scotese_noco2a | Yes | n | This is as scotese_02 but with no CO2 (or solar) variation. Extended a further 500 years.. More details of the simulations included in movie sequence can be found here |
| scotese_solara | Yes | n | This is as scotese_02 but with no CO2 variations but including solar constant change and extended for a further 1000 years.. More details of the simulations included in movie sequence can be found here |
| scotese_spinupa | Yes | n | This is as scotese_spinup, but extended for a further 500 years.. More details of the simulations included in movie sequence can be found here |
| ENSEMBLES | | | NEXT SECTION DESCRIBES ENSEMBLES |
| FAMOUS_LGM_01 | n | n | This is a physics parameter ensemble using the two-sweep version of FAMOUS. This is for LGM conditions and their are 100 simulations using a latin-hyper cube sampling of the parameters. Details of individual simulations list which parameters were changed for each simulation.. More details of the simulations included in ensemble sequence can be found here |
| FAMOUS_LGM_Extended_01 | n | n | This is a set of the best 13 simulations from the FAMOUS_LGM_01 ensemble. These have been run for 800 years (compared to 200 years for the original ensemble). The ordering of the simulations is related to their overall skill score as defined in fig 5 of the Gregoire et al 2011 paper.. More details of the simulations included in ensemble sequence can be found here |
| FAMOUS_LGM_Single_Pert_01 | n | n | This is an ensemble of simulations using the two-sweep version of FAMOUS. This is for LGM conditions and the physics parameters are changed one at a time. Details of individual simulations list which parameters were changed for each simulation.. More details of the simulations included in ensemble sequence can be found here |
| FAMOUS_Pre-Ind_01 | n | n | This is a physics parameter ensemble using the two-sweep version of FAMOUS. This is for pre-industrial conditions and their are 100 simulations using a latin-hyper cube sampling of the parameters. Details of individual simulations list which parameters were changed for each simulation.. More details of the simulations included in ensemble sequence can be found here |
| FAMOUS_Pre-Ind_Extended_01 | n | n | This is a set of the best 13 simulations from the FAMOUS_Pre-Ind_01 ensemble. These have been run for 800 years (compared to 200 years for the original ensemble). The ordering of the simulations is related to their overall skill score as defined in fig 5 of the Gregoire et al 2011 paper.. More details of the simulations included in ensemble sequence can be found here |
| FAMOUS_Pre-Ind_Single_Pert_01 | n | n | This is an ensemble of simulations using the two-sweep version of FAMOUS. This is for pre-industrial conditions and the physics parameters are changed one at a time. Details of individual simulations list which parameters were changed for each simulation.. More details of the simulations included in ensemble sequence can be found here |