de.dkrz.wdcc.iso2094442 series ECHOG_A15_PRI_MM Frank Kaspar Institut für Meteorologie der Freien Universität Berlin n/a author Prof. Dr. Ulrich Cubasch Institut für Meteorologie der Freien Universität Berlin n/a author Frank Kaspar Institut für Meteorologie der Freien Universität Berlin n/a pointOfContact Frank Kaspar Max-Planck-Institut fuer Meteorologie (MD) http://www.mad.zmaw.de/ originator Prof. Dr. Ulrich Cubasch Max-Planck-Institut fuer Meteorologie (MD) http://www.mad.zmaw.de/ originator 2022-04-25T04:57:57 ISO 19115 ISO 19139 / DKRZ ISO Simple Profile V1.0 http://doi.org/doi:10.1594/WDCC/ECHOG_A15_PRI_MM ECHOG_A15_PRI: 2000 year control run of preindustrial climate (DEKLIM-EEM project), monthly mean values ECHOG_A15_PRI: 2000 year control run of preindustrial climate (DEKLIM-EEM project), monthly mean values 2006-05-22 creation None ECHOG_A15_PRI: 2000 year control run of preindustrial climate (DEKLIM-EEM project), monthly mean values doi:10.1594/WDCC/ECHOG_A15_PRI_MM Frank Kaspar Max-Planck-Institut fuer Meteorologie (MD) http://www.mad.zmaw.de/ originator Prof. Dr. Ulrich Cubasch Max-Planck-Institut fuer Meteorologie (MD) http://www.mad.zmaw.de/ originator doi:10.1594/WDCC/ECHOG_A15_PRI_MM The purpose of the project DEKLIM-EEM is to reconstruct past interglacials based on proxy data and to understand the processes that are responsible for climatic changes during these interglacials by applying climate models. The data represent monthly average value of a simulation of the preindustrial climate (PRI) at around 1800 yr AD. Boundary conditions are equivalent to the other simulations of the project, apart from the concentration of greenhouse gases and orbital parameters: Greenhouse gas concentrations are derived from vostok ice core data: 280 ppmV CO2, 0.70 ppmV CH4 and 265 ppbV N2O. CFCs are set to zero. Orbital parameters have been calculated with the routine of Berger (1978): Eccentricity: 0.0167; Obliquity: 23.44; Perihelion: 282.7 The simulation has been started with the Levitus ocean climatology. ECHO-G is used as climate model. It is a coupled atmosphere/ocean model (ECHAM4_T30 + HOPE-E_T42er). The simulation was run on a NEC-SX6 (hurrikan). Atmospheric data were originally stored by the model every 12 hours. Ocean data is stored every month. As the boundary conditions are not time dependent, the time access is arbitrary. Related experiments: - ECHOG_A16_LIG control run, last interglacial (Eemian, 125 kyrBP, DEKLIM-EEM project), started with Levitus climatology, monthly mean values - ECHOG_A40_LGI: control run, last glacial inception (End of the Eemian, 115 kyrBP, DEKLIM-EEM project), started with Levitus climatology, monthly mean values. Frank Kaspar Institut für Meteorologie der Freien Universität Berlin n/a author Prof. Dr. Ulrich Cubasch Institut für Meteorologie der Freien Universität Berlin n/a author Frank Kaspar Institut für Meteorologie der Freien Universität Berlin n/a pointOfContact ECHAM4 theme HOPE theme control run theme glacial inception theme paleoclimate simulation theme ECHO-G theme interglacial theme eng 0.0 360.0 -90.0 90.0 0001-01-01 2023-12-30 24276 air_pressure_at_convective_cloud_top modelResult Pa air_pressure_at_sea_level modelResult Pa air_temperature modelResult K air_temperature modelResult K air_temperature modelResult K air_temperature modelResult K area_fraction modelResult fraction atmosphere_eastward_stress_due_to_gravity_wave_drag modelResult Pa atmosphere_horizontal_streamfunction modelResult m2 s-1 atmosphere_horizontal_velocity_potential modelResult m2 s-1 atmosphere_mass_content_of_cloud_liquid_water modelResult kg m-2 atmosphere_northward_stress_due_to_gravity_wave_drag modelResult Pa atmosphere_relative_vorticity modelResult s-1 atmosphere_water_vapor_content modelResult kg m-2 cloud_area_fraction modelResult fraction cloud_area_fraction modelResult fraction cloud_area_fraction_in_atmosphere_layer modelResult fraction cloud_liquid_water_mixing_ratio modelResult kg kg-1 conductive_heat_flux_through_sea modelResult W m-2 dew_point_temperature modelResult K dissipation_in_atmosphere_boundary_layer modelResult W m-2 divergence_of_wind modelResult s-1 eastward_wind modelResult m s-1 eastward_wind modelResult m s-1 effective modelResult K floating_ice_thickness modelResult m geopotential_height modelResult gpm glacier modelResult not filled gravity modelResult W m-2 humidity_mixing_ratio modelResult kg kg-1 land modelResult W m-2 land_binary_mask modelResult 1 lwe_convective_precipitation_rate modelResult m s-1 lwe_large_scale_precipitation_rate modelResult m s-1 lwe_snowfall_rate modelResult m s-1 lwe_thickness_of_surface_snow_amount modelResult m lwe_water_evaporation_rate modelResult m s-1 lwe_water_evaporation_rate modelResult m s-1 lwe_water_evaporation_rate modelResult m s-1 lwe_water_evaporation_rate modelResult m s-1 minus_one_times_surface_upwelling_longwave_flux_in_air modelResult W m-2 minus_one_times_surface_upwelling_shortwave_flux_in_air modelResult W m-2 minus_one_times_toa_outgoing_shortwave_flux modelResult W m-2 northward_wind modelResult m s-1 northward_wind modelResult m s-1 precipitation modelResult mm d-1 precipitation_rate modelResult m s-1 relative_humidity modelResult fraction residual_heat_flux_for_melting_sea modelResult W m-2 runoff_flux modelResult m s-1 sea modelResult K sea_ice_temperature modelResult K sea_surface_temperature modelResult K skin_reservoir_water_content modelResult m snow_temperature modelResult K soil_moisture_content modelResult m soil_temperature modelResult K soil_temperature modelResult K soil_temperature modelResult K soil_temperature modelResult K soil_temperature modelResult K surface_air_pressure modelResult Pa surface_albedo modelResult fraction surface_albedo modelResult fraction surface_albedo modelResult fraction surface_albedo modelResult fraction surface_downward_eastward modelResult Pa surface_downward_eastward_stress modelResult Pa surface_downward_eastward_stress modelResult Pa surface_downward_eastward_stress modelResult Pa surface_downward_latent_heat_flux modelResult W m-2 surface_downward_latent_heat_flux modelResult W m-2 surface_downward_latent_heat_flux modelResult W m-2 surface_downward_latent_heat_flux modelResult W m-2 surface_downward_northward_stress modelResult Pa surface_downward_northward_stress modelResult Pa surface_downward_northward_stress modelResult Pa surface_downward_northward_stress modelResult Pa surface_downward_sensible_heat_flux modelResult W m-2 surface_downward_sensible_heat_flux modelResult W m-2 surface_downward_sensible_heat_flux modelResult W m-2 surface_downward_sensible_heat_flux modelResult W m-2 surface_geopotential modelResult m2 s-2 surface_net_downward_longwave_flux modelResult W m-2 surface_net_downward_longwave_flux_assuming_clear_sky modelResult W m-2 surface_net_downward_radiation_flux modelResult W m-2 surface_net_downward_radiation_flux modelResult W m-2 surface_net_downward_shortwave_flux modelResult W m-2 surface_roughness_length modelResult m surface_roughness_length modelResult m surface_roughness_length modelResult m surface_roughness_length modelResult m surface_snow_melt_flux modelResult m s-1 surface_temperature modelResult K surface_temperature modelResult K surface_temperature modelResult K surface_temperature modelResult K tendency_of_surface_snow_amount modelResult m s-1 toa_net_downward_longwave_flux modelResult W m-2 toa_net_downward_longwave_flux_assuming_clear_sky modelResult W m-2 toa_net_downward_radiative_flux modelResult W m-2 toa_net_downward_shortwave_flux modelResult W m-2 total modelResult m s-1 ustar modelResult m3 s-3 water_flux_into_sea_water_from_rivers modelResult m3 s-1 wind_speed modelResult m s-1 wind_speed modelResult m s-1 GRIB WMO format GRIdded Binary data distributor Mb 65044 http://doi.org/doi:10.1594/WDCC/ECHOG_A15_PRI_MM series