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This catalogue entry provides Regional Climate Model (RCM) data on single levels from a number of experiments, models, domains, resolutions, ensemble members, time frequencies and periods computed over several regional domains all over the World in the framework of the Coordinated Regional Climate Downscaling Experiment (CORDEX). The term "single levels" is used to express that the variables are 2D-matrices computed on one vertical level which can be surface (or a level close to the surface) or a dedicated pressure level in the atmosphere. Multiple vertical levels are excluded from this catalogue entry.

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The term "region" in the CDS form refers to the different regional domains, which are as follows:

  • EUR: European domain from 27°N to 72°N and from 22°W to 45°E. The horizontal resolution for this domain is 0.11° x 0.11° (EUR-11).
  • MED: Mediterranean domain from 25°N to 52°N and from 21°W to 50°E. The horizontal resolutions for this domain are 0.11° x 0.11° (MED-11) and 0.44° x 0.44° (MED-44).
  • NAM: North-American domain from 12°N to 59°N and from 171°W to 24°W. The horizontal resolutions for this domain are 0.22° x 0.22° (NAM-22) and 0.44° x 0.44° (NAM-44).
  • ARC: Arctic domain from 46°N to 90°N and from 180°W  to 180°E. The horizontal resolutions for this domain are 0.22° x 0.22° (ARC-22) and 0.44° x 0.44° (ARC-44).
  • AFR: Africa domain from 45°S to 42°N and from 24°W to 60°E. The horizontal resolutions for this domain are 0.22° x 0.22° (AFR-22) and 0.44° x 0.44° (AFR-44).
  • SAM: South America domain from 52°S to 19°N and from 105°W to 17°W. The horizontal resolutions for this domain are 0.20° x 0.20° (SAM-20),0.22° x 0.22° (SAM-22) and 0.44° x 0.44° (SAM-44).

Additional details on each CORDEX geographical domain are available at https://cordex.org/domains/.

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Additionally, the uncertainty related to internal variability of the climate system is sampled by running several simulations with the same RCM-GCM combination. On the forms, these are indexed as separate ensemble members (the naming convention for ensemble members is available in the documentation). For each GCM, the same experiment was repeatedly done using slightly different conditions (like initial conditions or different physical parameterisations for instance) producing in that way an ensemble of experiments closely related. More details behind these sequential ensemble numbers will be is available in the detailed documentation.

On a general level in the CDS form for the RCM simulations “v” enumerates runs and not model versions. Runs numbers different from “v1” means new simulations relative to the first “v1” one. It might not mean a new version:

ANDRAS: we have to check, if this level of information is needed in this overview or that is enough in the documentation. Maybe one sentence about these "runs" is sufficient here.

GL: Agree with Andras. This paragraph burdens the overview.

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All known issues about the CORDEX data are documented through the ES-DOC Errata Service : https://errata.es-doc.org/.

The data are produced by the participating institutes of the EURO-CORDEX, Med-CORDEX projects and several national contributions to CORDEX. ANDRAS: this sentence might be extended in the view of the non-European data. GL: "several national contributions" is not enough ? I don't know if the non-European domains were part of similar consortiums as EURO-CORDEX or Med-CORDEX. I let Manuel and Grisha on this. Jose, would you check this, please?and modelling centres participating in the different CORDEX domains with partial support from different international and national contributions (including support from COPERNICUS for some of the EURO-CORDEX runs and for helping in the data curation and ESGF archiving process in some domains). 

Recommended search procedure: 

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DATA DESCRIPTION
Data typeGridded
Horizontal coverageDepends on the regional domain (grid projection may differ among RCMs)
Horizontal resolution0.11° x 0.11°, 0.20°x 0.20°, 0.22° x 0.22° or 0.44° x 0.44° depending on the region.
Vertical resolutionVariables are provided in one single level (which may differ among variables)
Temporal coverage

evaluation runs are from 1989 to 2008

historical runs are from 1951 to 2005

scenario runs are from 2006 to 2100

Temporal resolution3h, 6h, daily, monthly and seasonal
File formatNetCDF4
ConventionsClimate and Forecast (CF) Metadata Convention v1.6
VersionsLatest version of the data is provided.
Update frequencyRegular quarterly updates


MAIN
VARIABLES
NameShort nameUnitsDescription
Total run-off fluxmrrokg.m-2.s-1The mass of surface and sub-surface liquid water per unit area
2m temperaturetasKThe temperature of the air near the surface (or ambient temperature). The
and time, which drains from land. The
data represents the mean over the aggregation period at 2m above the surface.
Total cloud covercltDimensionlessTotal refers to the whole atmosphere column, as seen from the surface or the top of the atmosphere. Cloud cover refers to fraction of horizontal area occupied by clouds.
200hPa temperatureta200KThe temperature of the air at 200hPa. The data represents the mean over the aggregation period at 200hPa pressure level.
Surface upwelling shortwave radiationrsusW.m-2The upward shortwave radiative flux of energy from the surface per unit area
Minimum 2m temperature in the last 24 hourstasminKThe minimum temperature of the air near the surface. The data represents the daily minimum at 2m above the surface. 
Maximum 2m temperature in the last 24 hourstasmaxKThe maximum temperature of the air near the surface. The data represents the
mean over the aggregation period at
daily maximum at 2m above the surface.
Surface thermal radiation downwardrlds
Mean precipitation fluxprkg
W
.m-2.s-1The
downward longwave radiative flux of energy inciding on the surface from the above per unit area
deposition of water to the Earth's surface in the form of rain, snow, ice or hail. The precipitation flux is the mass of water per unit area and time. The data represents the mean over the aggregation period.
Surface solar radiation downwardsrsds
Mean evaporation fluxevspsblkg
W
.m-2.s-1The
downward shortwave radiative flux of energy
mass of surface and sub-surface liquid water per unit area
. The data
ant time, which evaporates from land. The data includes conversion to vapour phase from both the liquid and solid phase, i.e., includes sublimation, and represents the mean over the aggregation period
at the surface
.
Surface pressurepsPaThe air pressure at the lower boundary of the atmosphere. The
2m surface relative humidityhurs%

The relative humidity is the percentage ratio of the water vapour mass to the water vapour mass at the saturation point given the temperature at that location. The data represents the mean over the aggregation period at 2m above the surface.

OrographyorogmThe height above the geoid (being 0.0 over the ocean). The data is time-independent.Minimum 2m temperature in the last 24 hourstasminK
2m surface specific humidityhussDimensionlessThe amount of moisture in the air at 2m above the surface divided by the amount of air plus moisture at that location. The data represents the mean over the aggregation period at 2m above the surface.
Surface pressurepsPa

The air pressure at the lower boundary of the atmosphere. The data represents the mean over the aggregation period.

The minimum temperature of the air near the surface. The data represents the daily minimum at 2m above the surface. 

Mean sea level pressurepslPaThe air pressure at sea level. In regions where the Earth's surface is above sea level the surface pressure is used to compute the air pressure that would exist at sea level directly below given a constant air temperature from the surface to the sea level point. The data represents the mean over the aggregation period.
Mean precipitation fluxpr
10m Wind SpeedsfcWindm
kg.m-2
.s-1The
deposition
magnitude of
water to the Earth's surface in the form of rain, snow, ice or hail. The precipitation flux is the mass of water per unit area and time
the two-dimensional horizontal air velocity. The data represents the mean over the aggregation period at 10m above the surface.
Mean evaporation fluxevspsbl
Surface solar radiation downwardsrsdsW
kg
.m-2
.s-1The conversion of water from the Earth s surface in the form of rain, snow, ice or hail into vapor. The evaporation flux is the mass of water per unit area and time
The downward shortwave radiative flux of energy per unit area. The data represents the mean over the aggregation period at the surface.
Mean evaporation fluxevspsbl
Surface thermal radiation downwardrldsW
kg
.m-2
.s-1

The

mass of surface and sub-surface liquid water

downward longwave radiative flux of energy inciding on the surface from the above per unit area

ant time, which evaporates from land. The data includes conversion to vapour phase from both the liquid and solid phase, i.e., includes sublimation, and

. The data represents the mean over the aggregation period.

Maximum 2m temperature in the last 24 hourstasmaxK
Surface upwelling shortwave radiationrsusW.m-2

The upward shortwave radiative flux of energy from the surface per unit area

The maximum temperature of the air near the surface

. The data represents the

daily maximum at 2m above

mean over the aggregation period at the surface.

Land area fractionsftlf%The fraction (in percentage) of grid cell occupied by land surface. The data is time-independent.850hPa V-component of the windva850m.s-1The magnitude of the northward component of the wind. The data represents the mean over the aggregation period at 850hPa pressure level.850hPa U-component of the windua850m.s-1The magnitude of the eastward component of the wind. The
Total cloud covercltDimensionlessTotal refers to the whole atmosphere column, as seen from the surface or the top of the atmosphere. Cloud cover refers to fraction of horizontal area occupied by clouds. The data represents the mean over the aggregation period
at 850hPa pressure level
.
500hPa geopotentialzg500mThe gravitational potential energy per unit mass normalized by the standard gravity at 500hPa at the same latitude. The data represents the mean over the aggregation period at 500hPa pressure level.
200hPa v
10m u-component of
the
wind
va200
uasm.s-1The magnitude of the
northward
eastward component of the wind. The data represents the mean over the aggregation period at
200hPa pressure level
10m above the surface.
200hPa u
10m v-component of
the
wind
ua200
vasm.s-1The magnitude of
the eastward
the northward component of the wind. The data represents the mean over the aggregation period at
200hPa
10m above the surface.
200hPa
temperatureta200KThe temperature of the air at 200hPa. The
u-component of the windua200m.s-1

The magnitude of the eastward component of the wind. The data represents the mean over the aggregation period at 200hPa

pressure level.

above the surface.

200hPa v-component of the windva200
10m Wind SpeedsfcWind
m.s-1The magnitude of the
two-dimensional horizontal air velocity
northward component of the wind. The data represents the mean over the aggregation period at
10m above the surface
200hPa pressure level.
10m v
850hPa U-component of the wind
vas
ua850m.s-1The magnitude of
the northward
the eastward component of the wind. The data represents the mean over the aggregation period at
10m above the surface
850hPa pressure level.
10m u
850hPa V-component of the wind
uas
va850m.s-1The magnitude of the
eastward
northward component of the wind. The data represents the mean over the aggregation period at
10m above the surface.
850hPa pressure level.
Total run-off fluxmrrokg.m-2.s-1

The mass of surface and sub-surface liquid water per unit area and time, which drains from land. The

2m temperaturetasKThe temperature of the air near the surface (or ambient temperature). The

data represents the mean over the aggregation period

at 2m above the surface

.

2m surface specific humidityhussDimensionless
Mean evaporation fluxevspsblkg.m-2.s-1

The mass of surface and sub-surface liquid water per unit area ant time, which evaporates from land. The data includes conversion to vapour phase from both the liquid and solid phase, i.e., includes sublimation, and

The amount of moisture in the air at 2m above the surface divided by the amount of air plus moisture at that location. The data

represents the mean over the aggregation period

at 2m above the surface

.

2m surface relative humidity
Land area fractionsftlf
hurs
%

The relative humidity is the percentage ratio of the water vapour mass to the water vapour mass at the saturation point given the temperature at that location. The data represents the mean over the aggregation period at 2m above the surface.

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The fraction (in percentage) of grid cell occupied by land surface. The data is time-independent.
OrographyorogmThe height above the geoid (being 0.0 over the ocean). The data is time-independent.