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wdc-climate.de:3911359 eng; USA collection C6CMMIMIHhi Dr. Shingo Watanabe Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ pointOfContact 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 2021-01-25T00:00:00 ISO 19115 ISO 19115-2:2009 IPCC DDC: MIROC MIROC-ES2H model output prepared for CMIP6 CMIP historical 2023-07-28 publication 1 C6CMMIMIHhi doi:10.26050/WDCC/AR6.C6CMMIMIHhi Dr. Shingo Watanabe Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ Email: wnabe@jamstec.go.jp author Dr. Tomohiro Hajima Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ Email: hajima@jamstec.go.jp author Kengo Sudo Graduate School of Environmental Studies, Nagoya University http://www.env.nagoya-u.ac.jp/english/index.html Email: kengo@nagoya-u.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. Koji Ogochi Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ Email: ogochi@jamstec.go.jp author Takashi Arakawa Research Organization for Information Science and Technology not filled Email: arakawa@rist.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 Dr. Akihiko Ito National Institute for Environmental Studies http://www.nies.go.jp/index-e.html Email: itoh@nies.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. Yoshiki Komuro Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ Email: komuro@jamstec.go.jp author Dr. Tomoko Nitta Atmosphere and Ocean Research Institute, the University of Tokyo http://www.aori.u-tokyo.ac.jp/english/ Email: t_nitta@aori.u-tokyo.ac.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. Tomoo Ogura National Institute for Environmental Studies http://www.nies.go.jp/index-e.html Email: ogura@nies.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 Dr. Miho Sekiguchi Tokyo University of Marine Science and Technology https://www.kaiyodai.ac.jp/english/index.html Email: miho@kaiyodai.ac.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. Kaoru Tachiiri Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ Email: tachiiri@jamstec.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. Toshihiko Takemura Research Institute for Applied Mechanics, Kyushu University https://www.riam.kyushu-u.ac.jp/en/index-e.html Email: toshi@riam.kyushu-u.ac.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. 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 Kei Yoshimura Atmosphere and Ocean Research Institute, the University of Tokyo http://www.aori.u-tokyo.ac.jp/english/ Email: kei@aori.u-tokyo.ac.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 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-ES2H.historical' 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-ES2H climate model, released in 2018, includes the following components: aerosol: SPRINTARS6.0, atmos: CCSR AGCM (T85; 256 x 128 longitude/latitude; 81 levels; top level 0.004 hPa), atmosChem: CHASER4.0 (T42; 128 x 64 longitude/latitude; 81 levels; top level 0.004 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: 250 km, atmos: 250 km, atmosChem: 500 km, land: 250 km, ocean: 100 km, ocnBgchem: 100 km, seaIce: 100 km. Dr. Shingo Watanabe Japan Agency for Marine-Earth Science and Technology http://www.jamstec.go.jp/e/ pointOfContact 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-ES2H climate change historical 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 proleptic_gregorian 1850-01-16 1850-12-16 toa_incoming_shortwave_flux "shortwave" means shortwave radiation. "toa" means top of atmosphere. The TOA incoming shortwave flux is the radiative flux from the sun i.e. the "downwelling" TOA shortwave flux. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2 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 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 surface_upwelling_shortwave_flux_in_air The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2 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 surface_downwelling_longwave_flux_in_air surface_downwelling_longwave_flux_in_air [CF-Standard Name]; unit: W m-2 surface_downward_northward_stress The surface called "surface" means the lower boundary of the atmosphere. "Northward" indicates a vector component which is positive when directed northward (negative southward). "Downward" indicates a vector component which is positive when directed downward (negative upward). "Downward northward" indicates the ZY component of a tensor. A downward northward stress is a downward flux of northward momentum, which accelerates the lower medium northward and the upper medium southward. The surface downward stress is the windstress on the surface. [CF-Standard Name]; unit: Pa 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 specific_humidity "specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K surface_downward_eastward_stress The surface called "surface" means the lower boundary of the atmosphere. "Eastward" indicates a vector component which is positive when directed eastward (negative westward). "Downward" indicates a vector component which is positive when directed downward (negative upward). "Downward eastward" indicates the ZX component of a tensor. A downward eastward stress is a downward flux of eastward momentum, which accelerates the lower medium eastward and the upper medium westward. The surface downward stress is the windstress on the surface. [CF-Standard Name]; unit: Pa air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K toa_outgoing_shortwave_flux "shortwave" means shortwave radiation. "toa" means top of atmosphere. The TOA outgoing shortwave flux is the reflected and scattered solar radiative flux i.e. the "upwelling" TOA shortwave flux, sometimes called the "outgoing shortwave radiation" or "OSR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2 wind_speed Speed is the magnitude of velocity. 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.) The wind speed is the magnitude of the wind velocity.[CF-Standard Name]; unit: m s-1 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 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 geopotential_height Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K 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 water_evapotranspiration_flux Snow Evaporation Comment: Water here means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called 'sublimation'.) In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. Unless indicated in the cell_methods attribute, a quantity is assumed to apply to the whole area of each horizontal grid box. Previously, the qualifier where_type was used to specify that the quantity applies only to the part of the grid box of the named type. Names containing the where_type qualifier are deprecated and newly created data should use the cell_methods attribute to indicate the horizontal area to which the quantity applies. Used for mip era 'CMIP6' in CMOR MIP table(s): Table Eday, provided in frequency(s): day, and for Realm(s): land. Codelist created on 2019-02-01 from https://github.com/PCMDI/cmip6-cmor-tables (CMOR Version=3.4; table_date(s):14 December 2018) [CF-Standard Name]; unit: kg m-2 s-1 surface_upward_sensible_heat_flux The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called "turbulent" heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2 surface_air_pressure The surface called "surface" means the lower boundary of the atmosphere.[CF-Standard Name]; unit: Pa snowfall_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 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 toa_outgoing_longwave_flux "longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2 surface_upward_latent_heat_flux The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2 specific_humidity "specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1 surface_downwelling_shortwave_flux_in_air surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2 NetCDF 117 https://www.wdc-climate.de/ui/entry?acronym=C6CMMIMIHhi information collection