MiKlip

MiKlip (German: Mittelfristige Klima-Prognosen) is a German research program with the aim to develop a decadal climate prediction system (Marotzke et al., 2016). MiKlip is organized in 5 modules:



The global prediction system uses the Max-Planck Institute for Meteorology Earth-System Model MPI-ESM.

Within Module C the regionalization of the global predictions is performed with COSMO-CLM. During the first phase of MiKlip two additional RCMs (REMO and WRF) were also tested.

To estimate the skill of the predictions, large sets of initialized decadal hindcasts are performed, usually covering the period after 1960 with annually starting 10-year simulations. In contrast to the un-initialized simulations (historical simulations in CMIP) the hindcast derive their initial conditions from observations via assimilation experiments using atmospheric and oceanic re-analysis.

Four generations of hindcasts have been generated in MiKlip up to now:

1. baseline0 (= CMIP5)

2. baseline1

3. prototype

4. preop (pre operational)


Additionally, experiments have been performed to investigate the climate variability and trend over the whole 20th century for Europe, including re-analysis driven simulations based on NCEP 20CR and ERA20CC, MPI_ESM-LR decadal hindcasts and historical simulations.

Model domain

For the downscaling for Europe the EURO-CORDEX domain is used:

For Europe, the simulations are performed on a rotated grid with the pole at 162°W longitude and 39.25°N latitude. The domain covers approximately the region from about 22°W to 45°E longitude and 27°N to 72°N latitude. The resolutions applied are 0.44° (EUR-44) and 0.22° (EUR-22) and, for Central Europe, 0.0625° (CEUR-0625).

The recommended COSMO-CLM setup is used for the simulations:

Simulations performed with COSMO-CLM

Decadal Hindcasts

Ens. GenerationModel versionGridStarting yearsEnsemble members# Simulation years
baseline0COSMO-CLM4-8EUR-225 (1960, 1970, 1980 1990 2000)10500

COSMO-CLM4-8CEUR-06255 (1960, 1970, 1980 1990 2000)4200
baseline1COSMO-CLM4-8EUR-225 (1960, 1970, 1980 1990 2000)10500

COSMO-CLM4-8EUR-4457 (annual 1960 – 2016)105700
prototype                     COSMO-CLM5-0EUR-225 (1960, 1970, 1980 1990 2000)150
preopCOSMO-CLM5-0EUR-2257 (58) (annual 1960 – 2017)5 (10)2850 (5800)
20C_EURCOSMO-CLM5-0EUR-22100 (annual 1910 – 2009)3                    3000

Evaluation Simulations

Ens. GenerationModel versionGridPeriodEnsemble members# Simulation years
ERA40                         COSMO-CLM4-8EUR-22      1961 - 2002                            

1

42

ERAInterimCOSMO-CLM4-8EUR-221979 - 2010              132
ERA40+ERAInterimCOSMO-CLM4-8EUR-221961 - 2010149
ERA40+ERAInterimCOSMO-CLM4-8EUR-441961 - 2010149
ERA40+ERAInterimCOSMO-CLM5-0EUR-221961 - 2016156
NCEP 20CRCOSMO-CLM5-0EUR-22   1900 - 20093110
ERA20CFCOSMO-CLM5-0EUR-221900 - 20101111

Un-initialized (historical) simulations

GCMModel versionGridPeriodEnsemble members# Simulation years
MPI-ESM-LR (CMIP5)        COSMO-CLM4-8EUR-221961 - 2010149
MPI-ESM-LR (CMIP5)COSMO-CLM4-8EUR-441961 - 2010749
MPI-ESM-HR (CMIP5)                    COSMO-CLM5-0EUR-22

1900 – 2030 (1961-2030)

rcp45 after 2005
3 (2)131 (70)

Additional Experiments

NameProjectDetails

Africa

MiKlip I DEPARTURE

Decadal predictions of the West-African Monsoon and tropical Atlantic cyclogenesis

3 RCMs (COSMO-CLM4-8, REMO, WRF)

Resolution 0.44° (extended CORDEX Africa

4 Decades, 3 Members

Central America/North-Atlantic (CANA)

MiKlip I MesoTel2-way nested coupling of MPI-ESM and COSMO-CLM
Regionally coupled oceanMiKlip II C1-WP1Interactive coupling of COSMO-CLM5-0/NEMO for Mediterranean- Nordic, and Baltic-Sea

Alternative SVAT

MiKlip II C1-WP2Decadal hindcasts (preop generation) with COSMO-CLM5-0-Weg3D

Many more experiments have been performed including statistical dynamical downscaling with COSMO-CLM.

Contributing Partners MiKlip Phase II