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ICON NARVAL simulation over the tropical Atlantic for the ATL, BAR and AMA subdomains, the simulation day is 2013-12-01, extracted from NARVAL1 simulations

ICON 2.5 km simulations over the tropical Atlantic ([65W:15E],[10S:20N] for the months of December 2013 (NARVAL1 : 30 days) and August 2016 (NARVAL2 : 30 days).

The grid spacing, computed as the square root of the triangular grid cells, amounts to 2.5 km. In the vertical, a stretched vertical coordinate is used with 75 layers, whereby 12 layers are located in the first kilometer. The simulations are conducted for the months of December 2013 and July 2016. They are started every day at 00 UTC from the analysis of the European Centre for Medium-Range Weather Forecasts (ECMWF) and integrated for 36 hours. Boundary data are taken from the ECMWF forecasts and updated every 3 hours. At the bottom boundary, the Sea Surface Temperature (SST) is taken from the ECMWF analysis. It is kept fixed at its initial value during the 36-h integration period. The simulations were conducted using the ICOsahedral Non-hydrostatic (ICON) model (Zängl et al., 2015). Given the horizontal grid spacing, no convective parameterization is employed and convection is explicitly resolved by the bulk microphysics scheme that predicts cloud water, rain, snow, ice and graupel (Baldauf et al., 2011). The parameterizations for gravity wave drag and subgrid-scale orography are also switched off, otherwise the model employs the same parameterizations as the operational model version in use at the German Weather Service (DWD), see Zängl et al. (2015) and Klocke et al. (2017) for further details.

Simple

Date (Publication)
2021-01-14
Edition

1

Citation identifier
Narval1
Citation identifier
doi:10.26050/WDCC/Narval1
Principal investigator
  Max Planck Institute for Meteorology - Cathy Hohenegger
http://www.mpimet.mpg.de/
Author
  Max Planck Institute for Meteorology - Teacher-Researcher Nicolas Rochetin
http://www.mpimet.mpg.de/
Publisher
  WDC Climate at DKRZ
Point of contact
  Institut Pierre-Simon Laplace / Ecole Normale Supérieure - Teacher-Researcher Nicolas Rochetin
https://www.lmd.jussieu.fr/
Name

NetCDF

Use limitation

CC-BY-4.0: Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/

Language

eng; USA

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Begin date
2013-12-01
End date
2013-12-01
Distribution format
  • NetCDF ()

Transfer size
60889
OnLine resource
https://www.wdc-climate.de/ui/entry?acronym=Narval1
Hierarchy level
collection

Non quantitative attribute accuracy

Name of measure

n/a

Measure description

None

Attribute description
integral_of_surface_downward_latent_heat_flux_wrt_time
Descriptor

"integral_of_Y_wrt_X" means int Y dX. The data variable should have an axis for X specifying the limits of the integral as bounds. "wrt" means with respect to. The surface called "surface" means the lower boundary of the atmosphere. "Downward" indicates a vector component which is positive when directed downward (negative upward). 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: not filled

Attribute description
atmosphere_convective_available_potential_energy_wrt_surface
Descriptor

Convective(ly) available potential energy (often abbreviated CAPE) is a stability measure calculated by integrating the positive temperature difference between the surrounding atmosphere and a parcel of air lifted adiabatically from the surface to its equilibrium level. CAPE exists under conditions of potential instability, and measures the potential energy per unit mass that would be released by the unstable parcel if it were able to convect upwards to equilibrium. [CF-Standard Name]; unit: J kg-1

Attribute description
integral_of_surface_downward_sensible_heat_flux_wrt_time
Descriptor

"integral_of_Y_wrt_X" means int Y dX. The data variable should have an axis for X specifying the limits of the integral as bounds. "wrt" means with respect to. The surface called "surface" means the lower boundary of the atmosphere. "Downward" indicates a vector component which is positive when directed downward (negative upward). 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: not filled

Attribute description
mass_fraction_of_liquid_precipitation_in_air
Descriptor

"Mass fraction" is used in the construction "mass_fraction_of_X_in_Y", where X is a material constituent of Y. It means the ratio of the mass of X to the mass of Y (including X). A chemical species or biological group denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". "Liquid_precipitation" includes both "rain" and "drizzle". "Rain" means drops of water falling through the atmosphere that have a diameter greater than 0.5 mm. "Drizzle" means drops of water falling through the atmosphere that have a diameter typically in the range 0.2-0.5 mm. [CF-Standard Name]; unit: kg kg-1

Attribute description
virtual_potential_temperature
Descriptor

Virtual potential temperature; unit: K

Attribute description
integral_of_toa_net_longwave_radiation_wrt_time
Descriptor

TOA net thermal radiation acc.; unit: not filled

Attribute description
atmosphere_mass_content_of_graupel
Descriptor

"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including "content_of_atmosphere_layer" are used. Graupel consists of heavily rimed snow particles, often called snow pellets; often indistinguishable from very small soft hail except when the size convention that hail must have a diameter greater than 5 mm is adopted. Reference: American Meteorological Society Glossary http://glossary.ametsoc.org/wiki/Graupel . There are also separate standard names for hail. Standard names for "graupel_and_hail" should be used to describe data produced by models that do not distinguish between hail and graupel. [CF-Standard Name]; unit: kg m-2

Attribute description
air_pressure
Descriptor

air_pressure [CF-Standard Name]; unit: Pa

Attribute description
mass_fraction_of_snow_in_air
Descriptor

specific snow content [CF-Standard Name]; unit: kg kg-1

Attribute description
dew_point_temperature-at2m
Descriptor

Dew point temperature is the temperature at which a parcel of air reaches saturation upon being cooled at constant pressure and specific humidity.[CF-Standard Name-vertical_coordinate]; unit: K

Attribute description
cloud_ice_mixing_ratio
Descriptor

Mixing ratio of a parcel of ice in air is the ratio of the mass of ice to the mass of dry air. [CF-Standard Name]; unit: kg kg-1

Attribute description
cloud_liquid_water_mixing_ratio
Descriptor

Mixing ratio of a parcel of liquid water in air is the ratio of the mass of liquid water to the mass of dry air. [CF-Standard Name]; unit: kg kg-1

Attribute description
specific_humidity-at2m
Descriptor

"specific" means per unit mass. Specific humidity is the mass fraction of water

vapor in (moist) air.[CF-Standard Name-vertical_coordinate]; unit: kg kg-1

Attribute description
upward_air_velocity
Descriptor

vertical wind velocity A velocity is a vector quantity. "Upward" indicates a vector component which is positive when directed upward (negative downward). Upward air velocity is the vertical component of the 3D air velocity vector. [CF-Standard Name]; unit: m s-1

Attribute description
northward_wind
Descriptor

"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

Attribute description
air_temperature-at2m
Descriptor

Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name-vertical_coordinate]; unit: K

Attribute description
air_temperature
Descriptor

Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K

Attribute description
surface_temperature
Descriptor

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

Attribute description
integral_of_surface_moisture_flux_wrt_time
Descriptor

acc. moisture flux at surface; unit: not filled

Attribute description
eastward_wind-at10m
Descriptor

"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-vertical_coordinate]; unit: m s-1

Attribute description
lagrangian_tendency_of_air_pressure
Descriptor

"tendency_of_X" means derivative of X with respect to time. The Lagrangian tendency of a quantity is its rate of change following the motion of the fluid, also called the "material derivative" or "convective derivative". The Lagrangian tendency of air pressure, often called "omega", plays the role of the upward component of air velocity when air pressure is being used as the vertical coordinate. If the vertical air velocity is upwards, it is negative when expressed as a tendency of air pressure; downwards is positive.[CF-Standard Name]; unit: Pa s-1

Attribute description
air_density
Descriptor

[CF-Standard Name]; unit: kg m-3

Attribute description
atmosphere_mass_content_of_cloud_ice
Descriptor

Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. [CF-Standard Name]; unit: kg m-2

Attribute description
air_pressure_at_mean_sea_level
Descriptor

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

Attribute description
integral_of_surface_net_downward_shortwave_flux_wrt_time
Descriptor

integral_of_Y_wrt_X" means int Y dX. The data variable should have an axis for X specifying the limits of the integral as bounds. "wrt" means with respect to. The surface called "surface" means the lower boundary of the atmosphere. "Downward" indicates a vector component which is positive when directed downward (negative upward). Net downward radiation is the difference between radiation from above (downwelling) and radiation from below (upwelling). "Shortwave" means shortwave radiation. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: not filled

Attribute description
altitude (geometric height on half levels)
Descriptor

height (geometric height on half levels) [CF-Standard Name (cell_method)]; unit: m

Attribute description
northward_wind-at10m
Descriptor

"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-vertical_coordinate]; unit: m s-1

Attribute description
precipitation_amount
Descriptor

"Amount" means mass per unit area. "Precipitation" in the earths atmosphere means precipitation of water in all phases. [CF-Standard Name]; unit: kg m-2

Attribute description
atmosphere_convective_inhibition_wrt_surface
Descriptor

Convective inhibition is the amount of energy per unit mass required to overcome the negatively buoyant energy exerted by the environment on a parcel of air. Convective inhibition is often abbreviated as "CIN" or "CINH". It is calculated by integrating the negative temperature difference between the surrounding atmosphere and a parcel of air lifted adiabatically from the surface to its equilibrium level. [CF-Standard Name]; unit: J kg-1

Attribute description
atmosphere_mass_content_of_cloud_liquid_water
Descriptor

"Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. [CF-Standard Name]; unit: kg m-2

Attribute description
specific_humidity
Descriptor

"specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: kg kg-1

Attribute description
atmosphere_mass_content_of_water_vapor
Descriptor

atmosphere_mass_content_of_water_vapor [CF-Standard Name]; unit: kg m-2

Attribute description
cloud_area_fraction
Descriptor

"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: %

Attribute description
integral_of_surface_net_downward_longwave_flux_wrt_time
Descriptor

"integral_of_Y_wrt_X" means int Y dX. The data variable should have an axis for X specifying the limits of the integral as bounds. "wrt" means with respect to. The surface called "surface" means the lower boundary of the atmosphere. "Downward" indicates a vector component which is positive when directed downward (negative upward). Net downward radiation is the difference between radiation from above (downwelling) and radiation from below (upwelling). "Longwave" means longwave radiation. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: not filled

Attribute description
relative_humidity
Descriptor

relative_humidity [CF-Standard Name]; unit: %

Attribute description
relative_humidity-at2m
Descriptor

relative_humidity-at2m [CF-Standard Name-vertical_coordinate]; unit: %

Attribute description
integral_of_toa_net_downward_shortwave_flux_wrt_time
Descriptor

"integral_of_Y_wrt_X" means int Y dX. The data variable should have an axis for X specifying the limits of the integral as bounds. "wrt" means with respect to. "toa" means top of atmosphere. "Downward" indicates a vector component which is positive when directed downward (negative upward). Net downward radiation is the difference between radiation from above (downwelling) and radiation from below (upwelling). "Shortwave" means shortwave radiation. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: not filled

File identifier
wdc-climate.de:3880927 XML
Metadata language

eng; USA

Hierarchy level
collection
Hierarchy level name

Narval1

Date stamp
2020-09-24T15:58:05
Metadata standard name

ISO 19115

Metadata standard version

ISO 19115-2:2009

Point of contact
  Max Planck Institute for Meteorology - Cathy Hohenegger
http://www.mpimet.mpg.de/
Point of contact
  Institut Pierre-Simon Laplace / Ecole Normale Supérieure - Teacher-Researcher Nicolas Rochetin
https://www.lmd.jussieu.fr/
 
 

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