RD status of ALADINLAEF Y Wang ZAMG Austria

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R&D status of ALADIN-LAEF Y. Wang ZAMG, Austria With contribution from Bellus, Kann, Tascu,

R&D status of ALADIN-LAEF Y. Wang ZAMG, Austria With contribution from Bellus, Kann, Tascu, Weidle, Wittmann

LAEF: R&D Highlights • Added values of LAEF on ECMWF-EPS and higher resoltuion deterministic

LAEF: R&D Highlights • Added values of LAEF on ECMWF-EPS and higher resoltuion deterministic LAM • Studies on global EPS coupling • Atmospheric predictability related to surface conditions • Works towards larger domain and higher resolution • Statistical calibration • Application of LAEF

Added values of LAEF vs. ECMWF LAEF vs. ALADIN-AUSTRIA ALADIN-LAEF ECMWF-EPS Resolution 18 km;

Added values of LAEF vs. ECMWF LAEF vs. ALADIN-AUSTRIA ALADIN-LAEF ECMWF-EPS Resolution 18 km; 37 Levels TL 399; 62 Levels Ens. Size 16 50 Model ALADIN ECMWF-IFS ALADIN-LAEF ALADIN-AUSTRIA Resolution 18 km; 37 Levels 9. 6 km; 60 Levels Ensemble size 16 members 5 members (time lagged) Forecast Ensemble mean deterministic ALADIN-Austria: time lagged EPS

Studies on coupling with different global EPS What is the impact of inconsistent IC

Studies on coupling with different global EPS What is the impact of inconsistent IC and LBC perturbation? What is the impact of coupling different global EPS?

NCEP vs. ECMWF: CRPSS, surface variables 2 m T Precipitation 10 m Wind MSLP

NCEP vs. ECMWF: CRPSS, surface variables 2 m T Precipitation 10 m Wind MSLP

NCEP vs. ECMWF: CRPSS 500 h. Pa H 500 V 500 T 500 RH

NCEP vs. ECMWF: CRPSS 500 h. Pa H 500 V 500 T 500 RH 500

Atmospheric predictability related to surface conditions convective rainfall surface air temperature large scale rainfall

Atmospheric predictability related to surface conditions convective rainfall surface air temperature large scale rainfall

SURFPREC. EAU. CON VS SURFTEMPERATURE (Spread)

SURFPREC. EAU. CON VS SURFTEMPERATURE (Spread)

SURFPREC. EAU. GEC VS PROFTEMPERATURE (Spread)

SURFPREC. EAU. GEC VS PROFTEMPERATURE (Spread)

LAEF towards larger domain and higher resolution

LAEF towards larger domain and higher resolution

No progress, X pattern problem need to be totally solved!

No progress, X pattern problem need to be totally solved!

Statistical calibration: 10 m Wind

Statistical calibration: 10 m Wind

Application of LAEF in nowcasting INCA

Application of LAEF in nowcasting INCA

Next future: Ø Higher resolution of LAEF Ø Optimization of multi-physics, stochastic physics Ø

Next future: Ø Higher resolution of LAEF Ø Optimization of multi-physics, stochastic physics Ø Ensemble data assimilation Ø Predictability study on cloud permitting scale Ø AROME-EPS for WMO WWRP FROST-2014 Sochi-2014