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Model

ECHAM 6.3.05 (atmosphere)

JSBACH 3.20 20p1 (land)

Horizontal resolution and gridT127 (~100 km) on regular Gaussian grid
Atmosphere vertical resolutionL95
Top of atmosphere0.01 hPa
Soil levels (layers)

5

Layer 1: 0 - 0.065 m
Layer 2: 0.065 - 0.319 m
Layer 3: 0.319 - 1.232 m
Layer 4: 1.232 - 4.134 m
Layer 5: 4.134 - 9.834 m

Time step200 s

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Detailed documentation: MPIOM: Jungclaus et al., 2013

3. Boundary conditions - climate forcings

The forcing database for radiative parameters like ozone, aerosol and greenhouse gases is provided by CMIP6 for the historical period up to 2014. Afterwards, data of RCP 4.5 future scenarios is used.

Greenhouse gasesCMIP6
OzoneCMIP6
Tropospheric aerosolsMACv2
Volcanic aerosolsCMIP6
Solar forcingyes

Detailed documentation

For aerosols: Stevens, B., Fiedler, S., Kinne, S., Peters, K., Rast, S., Müsse, J., Smith, S. J., and Mauritsen, T.: MACv2-SP: a parameterization of anthropogenic aerosol optical properties and an associated Twomey effect for use in CMIP6, Geosci. Model Dev., 10, 433–452, https://doi.org/10.5194/gmd-10-433-2017, 2017. 

4. Initialization and initial condition (IC) perturbations

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HindcastForecast
Atmosphere initialization
ERA5ERA5T
Atmosphere IC perturbationsnonepertubation of diffusion in the uppermost layerpertubation of diffusion in the uppermost layernone

Land Initialization

indirect via atmosphere initializationindirect via atmosphere initialization
Land IC perturbationsnonenone
Soil moisture initializationindirect via atmosphere initializationindirect via atmosphere initialization
Snow initializationindirect via atmosphere initializationindirect via atmosphere initialization
Unperturbed control forecast?yesnoyesno

The assimilation for the atmosphere employs Newtonian relaxation of the reference data with the following variable-dependent relaxation times:

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7. Other relevant information

Interpolation details
Horizontal Interpolation
Vertical interpolation

8. Where to find more information

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