de.dkrz.wdcc.iso2094443
series
ECHOG_A40_LGI_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
2022-04-25T04:58:39
ISO 19115
ISO 19139 / DKRZ ISO Simple Profile V1.0
http://doi.org/doi:10.1594/WDCC/ECHOG_A40_LGI_MM
ECHOG_A40_LGI: Control Run for the Last Glacial Inception (End of the Eemian, 115 kyrBP, DEKLIM-EEM project),monthly mean values
ECHOG_A40_LGI: Control Run for the Last Glacial Inception (End of the Eemian, 115 kyrBP, DEKLIM-EEM project),monthly mean values
2006-05-22
creation
None
ECHOG_A40_LGI: Control Run for the Last Glacial Inception (End of the Eemian, 115 kyrBP, DEKLIM-EEM project), monthly mean values
doi:10.1594/WDCC/ECHOG_A40_LGI_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_A40_LGI_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 Last Glacial Inception (LGI) at 115000 years before present(End of the Eemian). Boundary conditions are the same as in the preindustrial control run (ECHOG_A15_PRI), apart from the concentration of greenhouse gases and orbital parameters:
Greenhouse gas concentrations are derived from vostok ice core data: 265
ppmV CO2, 0.52 ppmV CH4 and 270 ppbV N2O.
Orbital parameters have been calculated with the routine of Berger (1978):
Eccentricity: 0.0414; Obliquity: 22.41; Perihelion: 290.9
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_A15_PRI preindustrial control run (ca. 1800 A.D.; run a15), started with Levitus climatology.
ECHOG_A16_LIG control run, last interglacial (Eemian, 125 kyrBP; run a16), started with Levitus climatology.
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
2999-12-30
35988
air_pressure_at_convective_cloud_top
modelResult
Pa
air_pressure_at_sea_level
modelResult
Pa
air_temperature
modelResult
K
air_temperature
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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
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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
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m s-1
eastward_wind
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m s-1
effective
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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
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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
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W m-2
northward_wind
modelResult
m s-1
northward_wind
modelResult
m s-1
precipitation
modelResult
mm d-1
precipitation_rate
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m s-1
relative_humidity
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fraction
residual_heat_flux_for_melting_sea
modelResult
W m-2
runoff_flux
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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
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K
soil_temperature
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K
soil_temperature
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K
soil_temperature
modelResult
K
surface_air_pressure
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Pa
surface_albedo
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fraction
surface_albedo
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surface_albedo
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surface_albedo
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fraction
surface_downward_eastward
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Pa
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Pa
surface_downward_eastward_stress
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Pa
surface_downward_eastward_stress
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Pa
surface_downward_latent_heat_flux
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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
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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
96424
http://doi.org/doi:10.1594/WDCC/ECHOG_A40_LGI_MM
series