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Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology Meteo. Swiss

Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology Meteo. Swiss Status of the COSMO-1 configuration at Meteo. Swiss Guy de Morsier COSMO-GM-CORSO, Roma, 6. 9. 2011

Agenda • Motivation • Status of the ARPA-SIM collaboration • Domain • Outlook COSMO-GM-CORSO,

Agenda • Motivation • Status of the ARPA-SIM collaboration • Domain • Outlook COSMO-GM-CORSO, Roma, Sept. 2011 / Status of the COSMO-1 configuration at Meteo. Swiss Guy de Morsier 2

Motivation for COSMO-1 • Operational target is for 2015 • Why increase the grid

Motivation for COSMO-1 • Operational target is for 2015 • Why increase the grid resolution? - improve representation of forcing (e. g. topography, land use) - better capture non-linear interaction between different scales (e. g. convection) - improve use of observing systems in the assimilation step • Focus mainly on Alpine region and Alpine specific problems COSMO-GM-CORSO, Roma, Sept. 2011 / Status of the COSMO-1 configuration at Meteo. Swiss Guy de Morsier 3

Target: COSMO-1 suite in 2015 IFS boundary conditions 10 km grid size, 140 layers

Target: COSMO-1 suite in 2015 IFS boundary conditions 10 km grid size, 140 layers 4 x daily 8 x daily COSMO-1 + 24 hours forecasts 1 km grid size, 100 layers 1040 x 700 grid points COSMO-GM-CORSO, Roma, Sept. 2011 / Status of the COSMO-1 configuration at Meteo. Swiss Guy de Morsier 4

Target: COSMO-E suite in 2015 COSMO-E Var. EPS boundary conditions 20 km 2 x

Target: COSMO-E suite in 2015 COSMO-E Var. EPS boundary conditions 20 km 2 x daily COSMO-GM-CORSO, Roma, Sept. 2011 / Status of the COSMO-1 configuration at Meteo. Swiss 2 x daily +5 days forecasts 3 km grid size 21 members Guy de Morsier 5

Status of the ARPA-SIM collaboration √ Common domain • Test if a common configuration

Status of the ARPA-SIM collaboration √ Common domain • Test if a common configuration can be used and a common evaluation of results operated • Nesting strategy compare C-1 in C-7 with C-1 in C-2 • Decrease damping in upper layers cf. Wolfgang Langhans 1) • Tune the orographic filtering to the stability of the dynamics • Investigate the sensitivity to the asymptotic turbulent length scale and the vertical level distribution 1) Convergence of numerical simulations of linear hydrostatic gravity wave, March 11, 2011 COSMO-GM-CORSO, Roma, Sept. 2011 / Status of the COSMO-1 configuration at Meteo. Swiss Guy de Morsier 6

Large Alpine Domain 698 x 528 gridpoints CPU of COSMO-2 * 4 COSMO-GM-CORSO, Roma,

Large Alpine Domain 698 x 528 gridpoints CPU of COSMO-2 * 4 COSMO-GM-CORSO, Roma, Sept. 2011 / Status of the COSMO-1 configuration at Meteo. Swiss 300 m filter: max. gr. 18° C-1 with 750 m filter: 25° COSMO-2: 15° Guy de Morsier 9

Outlook • Choice of the orographic filtering should be adapted to the model dynamics!

Outlook • Choice of the orographic filtering should be adapted to the model dynamics! • Try to run unstable cases without horizontal diffusion • Set up an assimilation cycle for COSMO-1 • Regular runs from the assimilation cycle • Evaluate against COSMO-2 COSMO-GM-CORSO, Roma, Sept. 2011 / Status of the COSMO-1 configuration at Meteo. Swiss Guy de Morsier 11