Model: MPI-UW coupled ESM (ECHAM3/LSG2/HAMOCC3/LPJ) atmosphere: ECHAM3 AGCM, T21 resolution, 19 levels ocean: LSG2 OGCM, 64x64 resolution on Arakawa E, 22 levels marine biogeochemistry: HAMOCC3, resolution as ocean vegetation: LPJ, resolution as atmosphere ice sheets: prescribed, SICOPOLIS available periodically-synchronous coupling Reference: Mikolajewicz, U., Gröger, M., Maier-Reimer, E., Schurgers, G., Vizcaino, M. and Winguth, A. (2007): Long-term effects of anthropogenic CO2 emissions simulated with a complex earth system model. Climate Dynamics 28(6), 599-633, DOI:10.1007/s00382-006-0204-y. related publications: Schurgers, G., U. Mikolajewicz, M. Gröger, E. Maier-Reimer, M. Vizcaino and A. Winguth (): Long-term effects of biogeophysical and biogeochemical interactions between terrestrial biosphere and climate under anthropogenic climate change. Global and Planetary Change (acc.). Schurgers, G., U. Mikolajewicz, M. Gröger, E. Maier-Reimer, M. Vizcaino and A. Winguth (2006). Changes in terrestrial carbon storage during interglacials: a comparison between Eemian and Holocene. Climate of the Past 2, 205-220 www.clim-past.net/2/205/2006/cp-2-205-2006.html Schurgers, G. (2006): Long-term interactions between vegetation and climate -- Model simulations for past and future. Berichte zur Erdsystemforschung 27. http://www.mpimet.mpg.de/fileadmin/publikationen/Reports/BzE_27.pdf Winguth, A., Mikolajewicz, U., Gröger, M., Maier-Reimer, E., Schurgers, G., and Vizcaino, M. (2005): Centennial-scale interactions between the carbon cycle and anthropogenic climate change using a dynamic Earth system model Geophys. Res. Letters, 32,L23714, doi:10.1029/2005GL023681 Heinze, C., and E. Maier-Reimer, 1999, The Hamburg Oceanic Carbon Cycle Circulation Model Version "HAMOCC2s'' for long time integrations, Deutsches Klimarechenzentrum, Technical Report No. 20, 71 pp. For the basic experiment description see http://www.climate.uvic.ca/LTMIP - LSG and HAMOCC data have been remapped to a regular 64x32 grid (obs: remapping is not conservative!) - Carbon input in all cases (except hist) distributed over 12 months. - Weathering feedback not available (for consistency with experiment list 'w' is nevertheless used in experimentnames). - 'No sediment' runs have been performed with very small sediment pool (3GtC CaCO3). - In the experiments without interactive vegetation, the vegetation model is still integrated, sees the atmospheric pCO2, and modifies the land surface properties, but its carbon emissions to the atmosphere are suppressed. - Ensemble simulations (started with 1000 year difference) are denoted by the extra number behind the feedbackdescription. - CFC simulations have not been performed. time is given as YYYYMMDD, 360 days/year several points in the ocean are pure mixed-layer points (e.g. north of Greenland, Hudson Bay, Baltic etc.) without dynamic exchange with other grid points. Panama is closed. format of timeseries: column 1 year 2 pCO2(ppmV) 3 integrated carbon content ocean (PgC) 4 integrated alkalinity ocean (Peq) 5 CaCO3 sediment (PgC) 6 organic sediment (PgC) 7 carbon content atmosphere (PgC) for Hist and 2xPI only: 8 atmosphere-ocean carbon fluxes (PgC/year) 9 global mean surface DIC (kmol/kg) 10 global mean surface alkalinity {kmol/kg) contact: uwe.mikolajewicz(AT)zmaw.de