de.dkrz.wdcc.iso3887498 series LAT-SEASON-VOLCANIC_MPI-ESM-LR Dr. Zhihong Zhuo Freie Universität Berlin http://www.geo.fu-berlin.de/met/index.html author Dr. Ingo Kirchner Freie Universität Berlin http://www.geo.fu-berlin.de/met/index.html author Prof. Dr. Ulrich Cubasch Freie Universität Berlin http://www.geo.fu-berlin.de/met/index.html author Dr. Zhihong Zhuo Freie Universität Berlin http://www.geo.fu-berlin.de/met/index.html pointOfContact Dr. Zhihong Zhuo Freie Universität Berlin http://www.geo.fu-berlin.de/met/index.html originator 2022-03-12T04:25:17 ISO 19115 ISO 19139 / DKRZ ISO Simple Profile V1.0 http://doi.org/doi:10.26050/WDCC/LAT-SEASON-VOLCANIC_MPI-ESM-LR Different latitudinal volcanic eruption simulations in different seasons met.fu-berlin MPI-ESM-LR echam monthly Different latitudinal volcanic eruption simulations in different seasons met.fu-berlin MPI-ESM-LR echam monthly 2021-02-22 creation None Different latitudinal volcanic eruption simulations in different seasons met.fu-berlin MPI-ESM-LR echam monthly doi:10.26050/WDCC/LAT-SEASON-VOLCANIC_MPI-ESM-LR Dr. Zhihong Zhuo Freie Universität Berlin http://www.geo.fu-berlin.de/met/index.html originator doi:10.26050/WDCC/LAT-SEASON-VOLCANIC_MPI-ESM-LR In order to explore the sensitivity of the climate impact of volcanic eruptions to eruption season and latitude, we simulate volcanic eruptions at different latitudes and in different seasons with the Max Planck Institute Earth System Model (MPI-ESM). We use the same configuration of the MPI-ESM model as used for the historical simulation of CMIP6. An initial run is performed firstly (PINArst). Then we perform 23 and 10 control runs without any volcanic eruption (PINAref and PINAwRef). Two groups of three different latitudinal volcanic eruptions in boreal summer and winter are simulated. We perform 10-member simulations for each eruption case. 9 Tg of total sulfur injection magnitude is prescribed. The eruption latitudes are set to be 0° for the equatorial eruptions (PINAeq and PINAwEQ) and 30° N and 30° S for the northern and southern hemispheric eruptions (PINAnh, PINAwNH, PINAsh and PINAwNH), respectively. For the summer eruptions, the date is set to be the same as the 1991 Pinatubo eruption on June 15, 1991; for the winter eruptions, the date is set to be December 15, 1991. Dr. Zhihong Zhuo Freie Universität Berlin http://www.geo.fu-berlin.de/met/index.html author Dr. Ingo Kirchner Freie Universität Berlin http://www.geo.fu-berlin.de/met/index.html author Prof. Dr. Ulrich Cubasch Freie Universität Berlin http://www.geo.fu-berlin.de/met/index.html author Dr. Zhihong Zhuo Freie Universität Berlin http://www.geo.fu-berlin.de/met/index.html pointOfContact ECHAM6 theme MPI-ESM-LR theme stratospheric volcanic aerosol theme climate impact theme eng 0.0 358.125 -88.5722 88.5722 1966-01-01 1998-12-01 0 1986-01-01 1996-12-01 0 1990-01-01 1996-12-01 0 1991-01-01 1996-12-01 0 air_pressure_at_convective_cloud_top modelResult Pa air_pressure_at_convective_cloud_top modelResult Pa air_pressure_at_convective_cloud_top modelResult Pa air_pressure_at_convective_cloud_top modelResult Pa air_temperature modelResult K air_temperature modelResult K air_temperature modelResult K air_temperature modelResult K air_temperature modelResult K air_temperature modelResult K 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surface_downward_latent_heat_flux modelResult W/m2 surface_downward_latent_heat_flux modelResult W/m2 surface_downward_latent_heat_flux modelResult W/m2 surface_downward_latent_heat_flux modelResult W/m2 surface_downward_sensible_heat_flux modelResult W/m2 surface_downward_sensible_heat_flux modelResult W/m2 surface_downward_sensible_heat_flux modelResult W/m2 surface_downward_sensible_heat_flux modelResult W/m2 surface_geopotential modelResult m2/s2 surface_geopotential modelResult m2/s2 surface_geopotential modelResult m2/s2 surface_geopotential modelResult m2/s2 surface_net_downward_longwave_flux modelResult W/m2 surface_net_downward_longwave_flux modelResult W/m2 surface_net_downward_longwave_flux modelResult W/m2 surface_net_downward_longwave_flux modelResult W/m2 surface_net_downward_longwave_flux_assuming_clear_sky modelResult W/m2 surface_net_downward_longwave_flux_assuming_clear_sky modelResult W/m2 surface_net_downward_longwave_flux_assuming_clear_sky modelResult W/m2 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toa_net_downward_longwave_flux modelResult W/m2 toa_net_downward_longwave_flux modelResult W/m2 toa_net_downward_longwave_flux_assuming_clear_sky modelResult W/m2 toa_net_downward_longwave_flux_assuming_clear_sky modelResult W/m2 toa_net_downward_longwave_flux_assuming_clear_sky modelResult W/m2 toa_net_downward_longwave_flux_assuming_clear_sky modelResult W/m2 toa_net_downward_shortwave_flux modelResult W/m2 toa_net_downward_shortwave_flux modelResult W/m2 toa_net_downward_shortwave_flux modelResult W/m2 toa_net_downward_shortwave_flux modelResult W/m2 toa_net_downward_shortwave_flux_assuming_clear_sky modelResult W/m2 toa_net_downward_shortwave_flux_assuming_clear_sky modelResult W/m2 toa_net_downward_shortwave_flux_assuming_clear_sky modelResult W/m2 toa_net_downward_shortwave_flux_assuming_clear_sky modelResult W/m2 tropopause_air_pressure modelResult Pa tropopause_air_pressure modelResult Pa tropopause_air_pressure modelResult Pa tropopause_air_pressure modelResult Pa water_evaporation_flux modelResult kg(S) m-2 s-1 water_evaporation_flux modelResult kg(S) m-2 s-1 water_evaporation_flux modelResult kg(S) m-2 s-1 water_evaporation_flux modelResult kg(S) m-2 s-1 wind_speed modelResult m/s wind_speed modelResult m/s wind_speed modelResult m/s wind_speed modelResult m/s tar-File(s) tar-File(s) distributor Mb 162913 http://doi.org/doi:10.26050/WDCC/LAT-SEASON-VOLCANIC_MPI-ESM-LR series