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The CMIP6 data archive is distributed through the ESGF. A quality-controlled subset of CMIP6 global climate projection data are made available through the Climate Data Store (CDS) for the users of the Copernicus Climate Change Service (C3S). Dedicated ESGF data nodes are used for C3S in France (at IPSL) and in Germany (DKRZ).  Similarly, the decadal climate prediction project (DCPP) data in the Climate Data Store (CDS) are a targeted, quality-controlled subset of the DCPP commissioned by C3S.

The published datasets are the ones which took part on the C3S sectoral demonstrator service. This demonstrator provided decadal prediction products tailored to specific users from the agriculture, energy, infrastructure and insurance sectors (see details at https://climate.copernicus.eu/sectoral-applications-decadal-predictions) 

Decadal Climate Prediction Project Data in the CDS

DCPP Experiments

The CDS provides data access to two DCPP experiments: dcppA-hindcast which consists of retrospective decadal forecasts that can be used to assess historical decadal prediction skill, and dcppB-forecast which are experimental quasi-real-time decadal forecasts that form a basis for potential operational forecast production. For these DCPP experiments, each model performs multiple overlapping simulations that are initialised annually throughout the experiment. The dcppA-hindcast and dcppB-forecast experiments are further described in the table below. The DCPP experiment descriptions presented here are based on information harvested from Earth System Documentation (ES-DOC).

. The data were used in these demonstrators following processing procedures necessary to extract valid information (e.g., bias adjustment); details on this processing are available in the technical appendix at https://climate.copernicus.eu/sites/default/files/2021-09/Technical_appendix_2020.pdf. Any application - similar to or different from these examples - needs to consider and apply the required data processing with care.

Decadal Climate Prediction Project Data in the CDS

DCPP Experiments

The CDS provides data access to two DCPP experiments: dcppA-hindcast which consists of retrospective decadal forecasts that can be used to assess historical decadal prediction skill, and dcppB-forecast which are experimental quasi-real-time decadal forecasts that form a basis for potential operational forecast production. For these DCPP experiments, each model performs multiple overlapping simulations that are initialised annually throughout the experiment. The dcppA-hindcast and dcppB-forecast experiments are further described in the table below. The DCPP experiment descriptions presented here are based on information harvested from Earth System Documentation (ES-DOC).


Experiment Name

Experiment Long Name

Extended Description

dcppA-hindcast

hindcasts initialized from observations with historical forcing

dcppA-hindcast is a set of retrospective decadal forecasts (known as hindcasts) that are initialised every year mostly from 1960-2019 and performed with a

Experiment Name

Experiment Long Name

Extended Description

dcppA-hindcast

hindcasts initialized from observations with historical forcing

dcppA-hindcast is a set of retrospective decadal forecasts (known as hindcasts) that are initialised every year mostly from 1960-2019 and performed with a coupled atmosphere-ocean general circulation model (AOGCM).  The hindcasts begin in November to allow for DJF (December, January, February) seasonal averages to be calculated. There are 10 hindcasts for each start date and hindcasts run for 10 years.

The models running these hindcasts are initialised using observed data. Prior to the year 2020, the models are forced with historical conditions that are consistent with observations, these conditions include atmospheric composition, land use, volcanic aerosols and solar forcing. When hindcasts extend beyond 2020, the models are forced with future conditions from the ssp245 scenario from 2020 until the end of the simulation.

DCPP hindcast experiments can be used to assess and understand the historical decadal prediction skill of climate models.

dcppB-forecast

forecasts initialised from observations with ssp245 scenario forcing

dcppB-forecast is a set of quasi-real-time decadal forecasts that are initialised every year from 2019 in real time and ongoing (although only the data used in the secotoral demonstrator service is available from the CDS). The forecasts are performed with the same coupled atmosphere-ocean general circulation model (AOGCM), which was used to generate the hindcast data. The forecasts .  The hindcasts begin in November to allow for DJF (December, January, February) seasonal averages to be calculated. There are 10 forecasts hindcasts for each start date and forecasts hindcasts run for 10 years.

The models running these forecasts hindcasts are initialised using observed data. Prior to the year 2020, the models are forced with historical conditions that are consistent with observations, these conditions include atmospheric composition, land use, volcanic aerosols and solar forcing. When forecasts hindcasts extend beyond 2020, the models are forced with future conditions from the ssp245 scenario from 2020 until the end of the simulation.

DCPP forecast experiments form a basis for potential operational decadal forecast production.

Models

Data for the dcppA-hindcast and dcppB-forecast experiments published in the CDS are generated from simulations run by the models described in the table below. The model descriptions presented here are harvested from the dataset DOI pages held at the World Data Centre for Climate (WDCC), further model details can be found on the ES-DOC. The EC-Earth3, MPI-ESM1-2-HR, MPI-ESM1-2-LR and HadGEM3-GC31-MM models were configured with 360-day years (where every month has 30 days), whereas the CMCC-CM2-SR5 model was configured with a 365 day year (with an irregular number of days in each month). 

hindcast experiments can be used to assess and understand the historical decadal prediction skill of climate models.

dcppB-forecast

forecasts initialised from observations with ssp245 scenario forcing

dcppB-forecast is a set of quasi-real-time decadal forecasts that are initialised every year from 2019 in real time and ongoing (although only the data used in the secotoral demonstrator service is available from the CDS). The forecasts are performed with the same coupled atmosphere-ocean general circulation model (AOGCM), which was used to generate the hindcast data. The forecasts begin in November to allow DJF (December, January, February) seasonal averages to be calculated. There are 10 forecasts for each start date and forecasts run for 10 years.

The models running these forecasts are initialised using observed data. Prior to the year 2020, the models are forced with historical conditions that are consistent with observations, these conditions include atmospheric composition, land use, volcanic aerosols and solar forcing. When forecasts extend beyond 2020, the models are forced with future conditions from the ssp245 scenario from 2020 until the end of the simulation.

DCPP forecast experiments form a basis for potential operational decadal forecast production.

Models

Data for the dcppA-hindcast and dcppB-forecast experiments published in the CDS are generated from simulations run by the models described in the table below. The model descriptions presented here are harvested from the dataset DOI pages held at the World Data Centre for Climate (WDCC), further model details can be found on the ES-DOC. The EC-Earth3, MPI-ESM1-2-HR, MPI-ESM1-2-LR and HadGEM3-GC31-MM models were configured with 360-day years (where every month has 30 days), whereas the CMCC-CM2-SR5 model was configured with a 365 day year (with an irregular number of days in each month). 

Model

Centre

Description

EC-Earth3

EC Earth Consortium

The model used in climate research named EC Earth 3.3, released in 2019, includes the components:

  • atmos: IFS cy36r4 (TL255, linearly reduced Gaussian grid equivalent to 512 x 256 longitude/latitude; 91 levels; top level 0.01 hPa),
  • land: HTESSEL (land surface scheme built in IFS

Model

Centre

Description

EC-Earth3

EC Earth Consortium

The model used in climate research named EC Earth 3.3, released in 2019, includes the components:

  • atmos: IFS cy36r4 (TL255, linearly reduced Gaussian grid equivalent to 512 x 256 longitude/latitude; 91 levels; top level 0.01 hPa),
  • land: HTESSEL (land surface scheme built in IFS),
  • ocean: NEMO3.6 (ORCA1 tripolar primarily 1 deg with meridional refinement down to 1/3 degree in the tropics; 362 x 292 longitude/latitude; 75 levels; top grid cell 0-1 m),
  • seaIce: LIM3.

The model was run in native nominal resolutions: atmos: 100 km, land: 100 km, ocean: 100 km, seaIce: 100 km.

https://doi.org/10.22033/ESGF/CMIP6.227

CMCC-CM2-SR5

The Euro-Mediterranean Center on Climate Change (Centro Euro-Mediterraneo per I Cambiamenti Climatici, CMCC)

The model used in climate research named CMCC-CM2-SR5, released in 2016, includes the components:

  • aerosol: MAM3,
  • atmos: CAM5.3 (1deg; 288 x 192 longitude/latitude; 30 levels; top at ~2 hPa), land: CLM4.5 (BGC mode),
  • ocean: NEMO3.6 (ORCA1 tripolar primarly primarily 1 deg lat/lon with meridional refinement down to 1/3 degree in the tropics; 362 x 292 longitude/latitude; 50 vertical 75 levels; top grid cell 0-1 m),
  • seaIce: CICE4.0LIM3.

The model was run in native nominal resolutions: aerosol: 100 km, atmos: 100 km, land: 100 km, ocean: 100 km, seaIce: 100 km.

https://doi.org/10.22033/ESGF/CMIP6.1363227

MPICMCC-ESM1CM2-2-HRSR5

The German Weather Service (Deutscher Wetterdienst, DWD) / Max Planck Institute for Meteorology (MPI-M)Euro-Mediterranean Center on Climate Change (Centro Euro-Mediterraneo per I Cambiamenti Climatici, CMCC)

The model used in climate research named MPICMCC-ESM1.2CM2-HRSR5, released in 20172016, includes the components:

  • aerosol: noneMAM3, prescribed MACv2-SP,
  • atmos: ECHAM6CAM5.3 (spectral T1271deg; 384 288 x 192 longitude/latitude; 95 30 levels; top level 0.01 at ~2 hPa), land: JSBACH3.20,
  • landIce: none/prescribed,
  • CLM4.5 (BGC mode),
  • ocean: NEMO3.6 (ORCA1 tripolar primarly 1 deg lat/lon with meridional refinement down to 1/3 degree in the tropics; 362 x 292 longitude/latitude; 50 vertical ocean: MPIOM1.63 (tripolar TP04, approximately 0.4deg; 802 x 404 longitude/latitude; 40 levels; top grid cell 0-12 1 m),
  • ocnBgchem: HAMOCC6,
  • seaIce: thermodynamic (Semtner zero-layer) dynamic (Hibler 79) sea ice modelseaIce: CICE4.0.

The model was run in native nominal resolutions: aerosol: 100 km, atmos: 100 km, land: 100 km, landIce: none, ocean: 50 ocean: 100 km, ocnBgchem: 50 km, seaIce: 50 100 km.

https://doi.org/10.22033/ESGF/CMIP6.7681363

MPI-ESM1-2-LRHR

The German Weather Service (Deutscher Wetterdienst, DWD) / Max Planck Institute for Meteorology (MPI-M)

The model used in climate research named MPI-ESM1.2-LRHR, released in 2017, includes the components:

  • aerosol: none, prescribed MACv2-SP,
  • atmos: ECHAM6.3 (spectral T63T127; 384 x 192 x 96 longitude/latitude; 47 95 levels; top level 0.01 hPa),
  • land: JSBACH3.20,
  • landIce: none/prescribed,
  • ocean: MPIOM1.63 (bipolar GR1.5tripolar TP04, approximately 10.5deg4deg; 256 802 x 220 404 longitude/latitude; 40 levels; top grid cell 0-12 m),
  • ocnBgchem: HAMOCC6,
  • seaIce: thermodynamic (Semtner zero-layer) dynamic (Hibler 79) sea ice model.

The model was run in native nominal resolutions: aerosol: 250 100 km, atmos: 250 100 km, land: 250 100 km, landIce: none, ocean: 250 50 km, ocnBgchem: 250 50 km, seaIce: 250 50 km.

https://www.wdc-climate.de/ui/cmip6?input=CMIP6.DCPP.MPI-M.MPI-ESM1-2-LR

HadGEM3-GC31-MM

doi.org/10.22033/ESGF/CMIP6.768

MPI-ESM1-2-LR

The German Weather Service (Deutscher Wetterdienst, DWD) / Max Planck Institute for Meteorology (MPI-MMet Office Hadley Centre (MOHC)

The model used in climate research named HadGEM3MPI-GC3ESM1.12-N216ORCA025LR, released in 20162017, includes the components:

  • aerosol: UKCA-GLOMAP-modenone, prescribed MACv2-SP,
  • atmos: MetUM-HadGEM3-GA7.1 (N216; 432 x 324 ECHAM6.3 (spectral T63; 192 x 96 longitude/latitude; 85 47 levels; top level 85 km0.01 hPa),
  • land: JULES-HadGEM3-GL7.1JSBACH3.20,
  • landIce: none/prescribed,
  • ocean: NEMO-HadGEM3-GO6.0 (eORCA025 tripolar primarily 0.25 deg; 1440 x 1205 MPIOM1.63 (bipolar GR1.5, approximately 1.5deg; 256 x 220 longitude/latitude; 75 40 levels; top grid cell 0-1 12 m),
  • ocnBgchem: HAMOCC6,
  • seaIce: CICE-HadGEM3-GSI8 (eORCA025 tripolar primarily 0.25 deg; 1440 x 1205 longitude/latitude).thermodynamic (Semtner zero-layer) dynamic (Hibler 79) sea ice model.

The model was run in native nominal resolutions: aerosol: 100 250 km, atmos: 100 250 km, land: 100 250 km, landIce: none, ocean: 250 km, ocnBgchem: 25 250 km, seaIce: 25 250 km.

https://doi.org/10.22033/ESGF/CMIP6.456

Start-Date Ensembles

The DCPP experiments published in the CDS, are a suite of overlapping simulations that are initialised every year throughout the duration of the start-date range specified by the experiment. The simulations begin in November to allow for DJF (December, January, February) seasonal averages to be calculated. There are 10 simulations (ensemble members) for each start-date (called "Base year" in the CDS form), except for the MPI-ESM1-2-LR model which has 16 ensemble members.

The start-date ensemble is reflected in the DCPP data naming convention with the addition of a s<yyyy> start-date ensemble identifier. Please note that the conventional CMIP6 ripf ensemble identifiers are omitted for this particular dataset since all the ensemble members are concatenated into one file.

See some more more details in the File naming conventions and In-file metadata modifications sections below.

Practical details of the published data

In the table below some practical details of the data is shown including the base year (or start year) period covered and the number of ensemble members. For each start year there are (at least) 10 years of corresponding hindcast or forecast data available. Hindcast and forecast start years are not distinguished in the CDS form. Please note that the ensemble members are not available individually, but they are concatenated into one file while the data is downloaded, and generally users are encouraged to use all members instead of selecting one member of the predictions. 

...

www.wdc-climate.de/ui/cmip6?input=CMIP6.DCPP.MPI-M.MPI-ESM1-2-LR

HadGEM3-GC31-MM

Met Office Hadley Centre (MOHC)

The model used in climate research named HadGEM3-GC3.1-N216ORCA025, released in 2016, includes the components:

  • aerosol: UKCA-GLOMAP-mode,
  • atmos: MetUM-HadGEM3-GA7.1 (N216; 432 x 324 longitude/latitude; 85 levels; top level 85 km),
  • land: JULES-HadGEM3-GL7.1,
  • ocean: NEMO-HadGEM3-GO6.0 (eORCA025 tripolar primarily 0.25 deg; 1440 x 1205 longitude/latitude; 75 levels; top grid cell 0-1 m),
  • seaIce: CICE-HadGEM3-GSI8 (eORCA025 tripolar primarily 0.25 deg; 1440 x 1205 longitude/latitude).

The model was run in native nominal resolutions: aerosol: 100 km, atmos: 100 km, land: 100 km, ocean: 25 km, seaIce: 25 km.

https://doi.org/10.22033/ESGF/CMIP6.456

Start-Date Ensembles

The DCPP experiments published in the CDS, are a suite of overlapping simulations that are initialised every year throughout the duration of the start-date range specified by the experiment. The simulations begin in November to allow for DJF (December, January, February) seasonal averages to be calculated. There are 10 simulations (ensemble members) for each start-date (called "Base year" in the CDS form), except for the MPI-ESM1-2-LR model which has 16 ensemble members.

The start-date ensemble is reflected in the DCPP data naming convention with the addition of a s<yyyy> start-date ensemble identifier. Please note that the conventional CMIP6 ripf ensemble identifiers are omitted for this particular dataset since all the ensemble members are concatenated into one file.

See some more more details in the File naming conventions and In-file metadata modifications sections below.

Practical details of the published data

In the table below some practical details of the data is shown including the base year (or start year) period covered and the number of ensemble members. For each start year there are (at least) 10 years of corresponding hindcast or forecast data available. Hindcast and forecast start years are not distinguished in the CDS form. Please note that the ensemble members are not available individually, but they are concatenated into one file while the data is downloaded, and generally users are encouraged to use all members instead of selecting one member of the predictions. 


Hindcast start years*Forecast start years*Ensemble membersNominal resolutionMonthly variablesDaily variables
CMCC (Italy)1960 -2018 2019 - 202010100 kmNear surface air temperature, precipitation, sea level pressure---
EC-EARTH (Europe)1960 - 20182019 - 202010100 kmNear surface air temperature, precipitation, sea level pressure500 hPa geopotential height, daily maximum near surface air temperature, daily minimum near surface air temperature, near surface air temperature, precipitation, sea level pressure
HadGEM3 (UK)1960 - 20182019 - 202010100 kmNear surface air temperature, precipitation, sea level pressure500 hPa geopotential height, daily minimum near surface air temperature, precipitation
MPI-ESM1-2-HR (Germany)1960 - 2018---10100 kmNear surface air temperature, precipitation, sea level pressure500 hPa geopotential height, daily maximum near surface air temperature, daily minimum near surface air temperature, precipitation
MPI-ESM1-2-LR (Germany)1960 - 20182019 - 202116250 kmNear surface air temperature, precipitation, sea level pressureDaily maximum near surface air temperature, daily minimum near surface air temperature

*Note: Since hindcast and forecast data begins in November, the actual period the data covers includes only November and December for each start year, however the last year includes November and December. For example, for the 1960 start year, 1960 includes November and December and 1961 - 1970 have full coverage. 

Parameter listings

Data for the dcppA-hindcast experiments and the dcppB-forecast experiments will include parameters at monthly and daily resolution as described in the tables below. The parameter descriptions presented here are harvested from the CMIP6 Data Request via the CLIPC variable browser.

*Note: Since hindcast and forecast data begins in November, the actual period the data covers includes only November and December for each start year, however the last year includes November and December. For example, for the 1960 start year, 1960 includes November and December and 1961 - 1970 have full coverage. 

Parameter listings

Data for the dcppA-hindcast experiments and the dcppB-forecast experiments will include parameters at monthly and daily resolution as described in the tables below. The parameter descriptions presented here are harvested from the CMIP6 Data Request via the CLIPC variable browser.

Monthly Parameters

...

ESGF variable id

...

units

...

Standard name (CF)

...

Long name

...

Description

...

tas

...

K

...

air_temperature

...

Near-Surface Air Temperature

...

Temperature of air at 2m above the surface of land, sea or inland waters. 2m temperature is calculated by interpolating between the lowest model level and the Earth's surface, taking account of the atmospheric conditions.

...

pr

...

kg m-2 s-1

...

precipitation_flux

...

Precipitation

...

The sum of liquid and frozen water, comprising rain and snow, that falls to the Earth's surface. It is the sum of large-scale precipitation and convective precipitation. This parameter does not include fog, dew or the precipitation that evaporates in the atmosphere before it lands at the surface of the Earth. This variable represents amount of water per unit area and time.

...

psl

...

Pa

...

air_pressure_at_sea_level

...

Sea Level Pressure

...

The pressure (force per unit area) of the atmosphere at the surface of the Earth, adjusted to the height of sea level. It is a measure of the weight that all the air in a column vertically above a point on the Earth's surface would have, if the point were located at sea level. It is calculated over all surfaces - land, sea and inland water.

Daily Parameters

...

ESGF variable id

...

units

...

Standard name (CF)

...

Long name

...

Description

...

tasmin

...

K

...

air_temperature

...

Daily Minimum Near-Surface Air Temperature

...

Daily minimum temperature of air at 2m above the surface of land, sea or inland waters.

...

tasmax

...

K

...

air_temperature

...

Daily Maximum Near-Surface Air Temperature

...

Daily maximum temperature of air at 2m above the surface of land, sea or inland waters.

...

pr

...

kg m-2 s-1

...

precipitation_flux

...

Precipitation

...

The sum of liquid and frozen water, comprising rain and snow, that falls to the Earth's surface. It is the sum of large-scale precipitation and convective precipitation. This parameter does not include fog, dew or the precipitation that evaporates in the atmosphere before it lands at the surface of the Earth. This variable represents amount of water per unit area and time.

...

zg500

...

m

...

geopotential_height

...

Geopotential Height at 500hPa

...

Gravitational potential energy per unit mass normalised by the standard gravity at 500hPa at the same latitude.

INSTEAD, NEW TABLE PROPOSED

CDS parameter name

ESGF variable id

units

Standard name (CF)

Long name

Description

500 hPa geopotential height

zg500

m

geopotential_height

Geopotential Height at 500hPa

Gravitational potential energy per unit mass normalised by the standard gravity at 500hPa at the same latitude.

Daily maximum near-surface air temperature

tasmax

K

air_temperature

Daily Maximum Near-Surface Air Temperature

Daily maximum temperature of air at 2m above the surface of land, sea or inland waters.

Daily minimum near-surface air temperature 

tasmin

K

air_temperature

Daily Minimum Near-Surface Air Temperature

Daily minimum temperature of air at 2m above the surface of land, sea or inland waters.

Near-surface air temperature

tas

K

air_temperature

Near-Surface Air Temperature

Temperature of air at 2m above the surface of land, sea or inland waters. 2m temperature is calculated by interpolating between the lowest model level and the Earth's surface, taking account of the atmospheric conditions.

Precipitation

pr

kg m-2 s-1

precipitation_flux

Precipitation

The sum of liquid and frozen water, comprising rain and snow, that falls to the Earth's surface. It is the sum of large-scale precipitation and convective precipitation. This parameter does not include fog, dew or the precipitation that evaporates in the atmosphere before it lands at the surface of the Earth. This variable represents amount of water per unit area and time.

Sea level pressure

psl

Pa

air_pressure_at_sea_level

Sea Level Pressure

The pressure (force per unit area) of the atmosphere at the surface of the Earth, adjusted to the height of sea level. It is a measure of the weight that all the air in a column vertically above a point on the Earth's surface would have, if the point were located at sea level. It is calculated over all surfaces - land, sea and inland water.

...

World Climate Research Programme (2020) CMIP Phase 6 (CMIP6): Overview CMIP6 Experimental Design and Organization. Available at: https://www.wcrp-climate.org/wgcm-cmip/wgcm-cmip6 (Accessed: 2 November 2020).


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This document has been produced in the context of the Copernicus Climate Change Service (C3S).

The activities leading to these results have been contracted by the European Centre for Medium-Range Weather Forecasts, operator of C3S on behalf of the European Union (Delegation

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Agreement signed on 11/11/2014 and Contribution Agreement signed on 22/07/2021). All information in this document is provided "as is" and no guarantee or warranty is given that the information is fit for any particular purpose.

The users thereof use the information at their sole risk and liability. For the avoidance of all doubt , the European Commission and the European Centre for Medium - Range Weather Forecasts have no liability in respect of this document, which is merely representing the author's view.

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