wdc-climate.de:3926323 eng; USA collection C6CMMIMILam Dr. Tomohiro Hajima Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ pointOfContact Dr. Michio Kawamiya Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ pointOfContact 2020-03-18T00:00:00 ISO 19115 ISO 19115-2:2009 IPCC DDC: MIROC MIROC-ES2L model output prepared for CMIP6 CMIP amip 2023-07-28 publication 1 C6CMMIMILam doi:10.26050/WDCC/AR6.C6CMMIMILam Dr. Tomohiro Hajima Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ Email: hajima@jamstec.go.jp author Dr. Manabu Abe Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ Email: abemnb@jamstec.go.jp author Osamu Arakawa Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ Email: arakawa.osamu@jamstec.go.jp author Dr. Tatsuo Suzuki Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ Email: tsuzuki@jamstec.go.jp author Dr. Yoshiki Komuro Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ Email: komuro@jamstec.go.jp author Dr. Tomoo Ogura National Institute for Environmental Studies http://www.nies.go.jp/index-e.html Email: ogura@nies.go.jp author Dr. Koji Ogochi Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ Email: ogochi@jamstec.go.jp author Dr. Michio Watanabe Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ Email: michiow@jamstec.go.jp author Dr. Akitomo Yamamoto Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ Email: akitomo@jamstec.go.jp author Dr. Hiroaki Tatebe Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ Email: tatebe@jamstec.go.jp author Maki A. Noguchi Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ Email: macky@jamstec.go.jp author Dr. Rumi Ohgaito Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ Email: ohgaito@jamstec.go.jp author Akinori Ito Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ Email: akinorii@jamstec.go.jp author Dr. Dai Yamazaki Institute of Industrial Science, the University of Tokyo https://www.iis.u-tokyo.ac.jp/en/ Email: yamadai@rainbow.iis.u-tokyo.ac.jp author Dr. Akihiko Ito National Institute for Environmental Studies http://www.nies.go.jp/index-e.html Email: itoh@nies.go.jp author Dr. Kumiko Takata National Institute for Environmental Studies http://www.nies.go.jp/index-e.html Email: takata.kumiko@nies.go.jp author Dr. Shingo Watanabe Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ Email: wnabe@jamstec.go.jp author Dr. Michio Kawamiya Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ Email: kawamiya@jamstec.go.jp author Dr. Kaoru Tachiiri Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ Email: tachiiri@jamstec.go.jp author WDC Climate at DKRZ publisher These data include the subset used by IPCC AR6 WGI authors of the datasets originally published in ESGF for 'CMIP6.CMIP.MIROC.MIROC-ES2L.amip' with the full Data Reference Syntax following the template 'mip_era.activity_id.institution_id.source_id.experiment_id.member_id.table_id.variable_id.grid_label.version'. The MIROC-ES2L climate model, released in 2018, includes the following components: aerosol: SPRINTARS6.0, atmos: CCSR AGCM (T42; 128 x 64 longitude/latitude; 40 levels; top level 3 hPa), land: MATSIRO6.0+VISIT-e ver.1.0, ocean: COCO4.9 (tripolar primarily 1deg; 360 x 256 longitude/latitude; 63 levels; top grid cell 0-2 m), ocnBgchem: OECO ver.2.0; NPZD-type with C/N/P/Fe/O cycles, seaIce: COCO4.9. The model was run by the JAMSTEC (Japan Agency for Marine-Earth Science and Technology, Kanagawa 236-0001, Japan), AORI (Atmosphere and Ocean Research Institute, The University of Tokyo, Chiba 277-8564, Japan), NIES (National Institute for Environmental Studies, Ibaraki 305-8506, Japan), and R-CCS (RIKEN Center for Computational Science, Hyogo 650-0047, Japan) (MIROC) in native nominal resolutions: aerosol: 500 km, atmos: 500 km, land: 500 km, ocean: 100 km, ocnBgchem: 100 km, seaIce: 100 km. Dr. Tomohiro Hajima Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ pointOfContact Dr. Michio Kawamiya Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ pointOfContact NetCDF CMIP CMIP6 IPCC IPCC-AR6 IPCC-DDC MIROC MIROC-ES2L amip climate change model-output CC-BY-4.0: Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ eng; USA 0.0 360.0 -90.0 90.0 gregorian 1979-01-16 2014-12-16 precipitation_flux In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K atmosphere_mass_content_of_water_vapor atmosphere_mass_content_of_water_vapor [CF-Standard Name]; unit: kg m-2 surface_snow_amount surface_snow_amount [CF-Standard Name]; unit: kg m-2 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K northward_wind "Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1 surface_net_downward_mass_flux_of_carbon_dioxide_expressed_as_carbon_due_to_all_land_processes surface_net_downward_mass_flux_of_carbon_dioxide_expressed_as_carbon_due_to_all_land_processes [CF-Standard Name]; unit: kg m-2 s-1 eastward_wind "Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1 surface_temperature The surface called "surface" means the lower boundary of the atmosphere. The surface temperature is the (skin) temperature at the interface, not the bulk temperature of the medium above or below. [CF-Standard Name]; unit: K soil_temperature Soil temperature is the bulk temperature of the soil, not the surface (skin) temperature. [CF-Standard Name]; unit: K cloud_area_fraction "X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K air_pressure_at_mean_sea_level Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL. Air pressure is the force per unit area which would be exerted when the moving gas molecules of which the air is composed strike a theoretical surface of any orientation. "Mean sea level" means the time mean of sea surface elevation at a given location over an arbitrary period sufficient to eliminate the tidal signals. [CF-Standard Name]; unit: Pa NetCDF 1839 https://www.wdc-climate.de/ui/entry?acronym=C6CMMIMILam information collection