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wdc-climate.de:3952056 eng; USA collection C6CMMRME0am Dr. Seiji Yukimoto Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Dr. Tsuyoshi Koshiro Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Dr. Hideaki Kawai Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Dr. Naga Oshima Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Dr. Kohei Yoshida Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Dr. Shogo Urakawa Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Hiroyuki Tsujino Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Makoto Deushi Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Taichu Tanaka Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Masahiro Hosaka Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Hiromasa Yoshimura Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Eiki Shindo Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Ryo Mizuta Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Dr. Masayoshi Ishii Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Yukimasa Adachi Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact 2019-06-03T00:00:00 ISO 19115 ISO 19115-2:2009 IPCC DDC: MRI MRI-ESM2.0 model output prepared for CMIP6 CMIP amip 2023-07-28 publication 1 C6CMMRME0am doi:10.26050/WDCC/AR6.C6CMMRME0am Dr. Seiji Yukimoto Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html Email: yukimoto@mri-jma.go.jp author Dr. Tsuyoshi Koshiro Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html Email: tkoshiro@mri-jma.go.jp author Dr. Hideaki Kawai Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html Email: h-kawai@mri-jma.go.jp author Dr. Naga Oshima Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html Email: oshima@mri-jma.go.jp author Dr. Kohei Yoshida Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html Email: kyoshida@mri-jma.go.jp author Dr. Shogo Urakawa Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html Email: surakawa@mri-jma.go.jp author Hiroyuki Tsujino Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html Email: htsujino@mri-jma.go.jp author Makoto Deushi Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html Email: mdeushi@mri-jma.go.jp author Taichu Tanaka Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html Email: yatanaka@mri-jma.go.jp author Masahiro Hosaka Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html Email: mhosaka@mri-jma.go.jp author Hiromasa Yoshimura Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html Email: hyoshimu@mri-jma.go.jp author Eiki Shindo Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html Email: eishindo@mri-jma.go.jp author Ryo Mizuta Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html Email: rmizuta@mri-jma.go.jp author Dr. Masayoshi Ishii Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html Email: maish@mri-jma.go.jp author Atsushi Obata Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html Email: aobata@mri-jma.go.jp author Yukimasa Adachi Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html Email: yadachi@mri-jma.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.MRI.MRI-ESM2-0.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 MRI-ESM2.0 climate model, released in 2017, includes the following components: aerosol: MASINGAR mk2r4 (TL95; 192 x 96 longitude/latitude; 80 levels; top level 0.01 hPa), atmos: MRI-AGCM3.5 (TL159; 320 x 160 longitude/latitude; 80 levels; top level 0.01 hPa), atmosChem: MRI-CCM2.1 (T42; 128 x 64 longitude/latitude; 80 levels; top level 0.01 hPa), land: HAL 1.0, ocean: MRI.COM4.4 (tripolar primarily 0.5 deg latitude/1 deg longitude with meridional refinement down to 0.3 deg within 10 degrees north and south of the equator; 360 x 364 longitude/latitude; 61 levels; top grid cell 0-2 m), ocnBgchem: MRI.COM4.4, seaIce: MRI.COM4.4. The model was run by the Meteorological Research Institute, Tsukuba, Ibaraki 305-0052, Japan (MRI) in native nominal resolutions: aerosol: 250 km, atmos: 100 km, atmosChem: 250 km, land: 100 km, ocean: 100 km, ocnBgchem: 100 km, seaIce: 100 km. Dr. Seiji Yukimoto Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Dr. Tsuyoshi Koshiro Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Dr. Hideaki Kawai Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Dr. Naga Oshima Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Dr. Kohei Yoshida Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Dr. Shogo Urakawa Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Hiroyuki Tsujino Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Makoto Deushi Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Taichu Tanaka Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Masahiro Hosaka Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Hiromasa Yoshimura Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Eiki Shindo Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Ryo Mizuta Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Dr. Masayoshi Ishii Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact Yukimasa Adachi Meteorological Research Institute http://www.mri-jma.go.jp/Welcome.html pointOfContact NetCDF CMIP CMIP6 IPCC IPCC-AR6 IPCC-DDC MRI MRI-ESM2-0 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 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K 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 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 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 toa_outgoing_shortwave_flux_assuming_clear_sky toa_outgoing_shortwave_flux_assuming_clear_sky [CF-Standard Name]; unit: W m-2 atmosphere_mass_content_of_water_vapor atmosphere_mass_content_of_water_vapor [CF-Standard Name]; unit: kg 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 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K surface_snow_amount surface_snow_amount [CF-Standard Name]; unit: kg m-2 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 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 surface_downwelling_shortwave_flux_in_air surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2 soil_temperature Soil temperature is the bulk temperature of the soil, not the surface (skin) temperature. [CF-Standard Name]; unit: K toa_outgoing_longwave_flux_assuming_clear_sky A phrase assuming_condition indicates that the named quantity is the value which would obtain if all aspects of the system were unaltered except for the assumption of the circumstances specified by the condition. "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 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 mole_fraction_of_carbon_dioxide_in_air Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: mol mol-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 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K 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_upwelling_longwave_flux_in_air The surface called "surface" means the lower boundary of the atmosphere. "longwave" means longwave 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 NetCDF 31719 https://www.wdc-climate.de/ui/entry?acronym=C6CMMRME0am information collection