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M. Baldauf, U. Blahak (DWD)1 Status report of WG2 - Numerics and Dynamics COSMO General Meeting 02-05 Sept. 2013, Sibiu M. Baldauf, U. Blahak (DWD)

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Presentation on theme: "M. Baldauf, U. Blahak (DWD)1 Status report of WG2 - Numerics and Dynamics COSMO General Meeting 02-05 Sept. 2013, Sibiu M. Baldauf, U. Blahak (DWD)"— Presentation transcript:

1 M. Baldauf, U. Blahak (DWD)1 Status report of WG2 - Numerics and Dynamics COSMO General Meeting 02-05 Sept. 2013, Sibiu M. Baldauf, U. Blahak (DWD)

2 Outline Recent developments in the new fast waves solver New Bott advection operator with deformational correction Higher order discretization WG2 publications Science plan contributions from WG2 M. Baldauf, U. Blahak (DWD)2

3 3 Recent developments in the new fast waves solver M. Baldauf (DWD) New fast waves solver is available since COSMO 4.24 Runs operationally in COSMO-DE, -DE-EPS, -EU at DWD since 16 Jan. 2013 COSMO 4.27: additional options analogous to the old FW solver: optional use of the upper boundary damping layer by Klemp et al. (2008) lw_freeslip can be used new version of the radiative lateral boundary condition COSMO 4.28: 3D divergence damping now works correctly Bug fixes: in case of ldyn_bbc=.true.: Reproducibility is achieved Adaptation to the newer formulation of the buoyancy term Bug fix in the water loading contribution of the buoyancy term

4 M. Baldauf, U. Blahak (DWD)4 Bug fix in the water loading contribution of the buoancy term Moisture correction in ideal gas law: (water loading) RK-scheme with new fast waves solver: 4.27:moisture variables q v, q c, … in q x at timelevel nnew 4.28:moisture variables q v, q c, … in q x at timelevel nnow reason: during the RK-scheme nnew still means ‚old‘ for the moisture variables! This bug fix is important in strongly convective situations

5 COSMO-DE, 20.06.2013, 12 UTC run 1h precipitation sum ‚nnew‘Radar‚nnow‘ Front coming in at evening; convergence line during afternoon with heavy precipitation M. Baldauf, U. Blahak (DWD)5

6 ‚nnew‘Radar‚nnow‘ COSMO-DE, 20.06.2013, 12 UTC run 1h precipitation sum

7 ‚nnew‘Radar‚nnow‘ COSMO-DE, 20.06.2013, 12 UTC run 1h precipitation sum M. Baldauf, U. Blahak (DWD)7

8 ‚nnew‘Radar‚nnow‘ COSMO-DE, 20.06.2013, 12 UTC run 1h precipitation sum M. Baldauf, U. Blahak (DWD)8

9 ‚nnew‘Radar‚nnow‘ COSMO-DE, 20.06.2013, 12 UTC run 1h precipitation sum M. Baldauf, U. Blahak (DWD)9

10 ‚nnew‘Radar‚nnow‘ COSMO-DE, 20.06.2013, 12 UTC run 1h precipitation sum M. Baldauf, U. Blahak (DWD)10

11 ‚nnew‘Radar‚nnow‘ COSMO-DE, 20.06.2013, 12 UTC run 1h precipitation sum M. Baldauf, U. Blahak (DWD)11

12 ‚nnew‘Radar‚nnow‘ COSMO-DE, 20.06.2013, 12 UTC run 1h precipitation sum M. Baldauf, U. Blahak (DWD)12

13 ‚nnew‘Radar‚nnow‘ COSMO-DE, 20.06.2013, 12 UTC run 1h precipitation sum M. Baldauf, U. Blahak (DWD)13

14 COSMO-DE, 20.06.2013, 12 UTC run 24h precipitation sum ‚nnew‘Radar‚nnow‘ M. Baldauf, U. Blahak (DWD)14

15 M. Baldauf, U. Blahak (DWD)15 Synop-Verifikation COSMO-DE Parallel COSMO-DE Routine

16 M. Baldauf, U. Blahak (DWD)16 Synop-Verifikation COSMO-DE Parallel COSMO-DE Routine

17 M. Baldauf, U. Blahak (DWD)17 Synop-Verifikation COSMO-EU Parallel COSMO-EU Routine

18 M. Baldauf, U. Blahak (DWD)18 Synop-Verifikation COSMO-EU Parallel COSMO-EU Routine

19 M. Baldauf, U. Blahak (DWD)19 Synop-Verifikation COSMO-EU Parallel COSMO-EU Routine

20 M. Baldauf, U. Blahak (DWD)20 Synop-Verifikation COSMO-EU Parallel COSMO-EU Routine

21 M. Baldauf, U. Blahak (DWD)21 New Bott advection operator with deformational correction W. Schneider, A. Bott (Univ. Bonn), U. Blahak (DWD)

22 M. Baldauf, U. Blahak (DWD) Bott scheme with deformational correction: basic idea 22 Strain deformation terms Their sum = divergence Properties:  Exactly consistent  Exactly conserving  Almost shape preserving  Positive definite  Bonn group claims:  Increased stability in steep terrain  No need for „true strang splitting“ any more

23 M. Baldauf, U. Blahak (DWD) Bott scheme with deformational correction: idealized COSMO WK82 23 Accumulated rain after 4 h New BottDiff Bott2 – new BottDiff Bott2_Strang – new Bott Current implementation: Coupling of separate Bonn code by Werner Schneider, vectorization by Ulrich Blahak. Good for current testing, but new implementation based on the existing COSMO routines of the Bott schemes would be desireable!

24 Higher Order Spatial Schemes in COSMO Model: Stability and Convergence tests Jack Ogaja and Andreas Will, BTU Cottbus, Germany i.e. U-momentum balance equation advC4p2v2: 4 th order cosmo adv + new fast waves solver advN4p4v2: new 4 th order adv + new fast waves solver (4 th order) advS4p4v2: symmetric 4 th order adv + new fast waves solver (4 th order); stencil has only half width! advS4p4v2: symmetric 4 th order adv + new fast waves solver (2 nd order) Different spatial schemes tested in COSMO-4.24  advS4p4v2 and advS4p2v2 conserves both 1 st and 2 nd moments of the advected quantity when the continuity equation is satisfied. ( Morinishi et al. JCP 1998, 2010 )

25 advC4p2v2, after 8hrs advN4p4v2, after 8hrs Atmosphere at rest test case (TST01) h max = 3000m u 0 = 0m/s, a = 10000m N = 0.01 s -1, Dx = 1000m ie_tot = 500, ke_tot = 500 Reduced magnitude of spurious solution in the lower cells after 8hrs of simulation using advN4p4v2. Positive effect of 4 th order discretisation of pressure gradient term in advN4p4v2

26 Fig1: Time series of L 1 error norm for w of TST01, h max =1km and dx=1km, atmosphere at rest, no diffusion Results: Development of mean absolute difference error (L 1 ) with time exhibits different levels of stability for the four schemes. advS4p4v2 and advS4p2v2 show improved stability, probably due to the conservation of kinetic energy by the advection scheme. advN4p4v2 and advS4p4v2 reveal improved accuracy before the instability mechanism (i.e. before approx. 16hrs) is dominating the result, due to 4 th order convergence Fig2: Convergence plot of w for the four schemes after 1 hr of simulation of TST01, with h max =1km. Reference: dx=125m Results: Mean absolute difference error (L 1 ) converges faster (near 4 th order) in advN4p4v2 and advS4p4v2. advC4p2v2, and advS4p2v2 are 2 nd order convergent due to 2 nd order discretisation of pressure gradient term and 2 nd order interpolations in the advection term of advC4p2v22

27 M. Baldauf, U. Blahak (DWD)27 WG2 publications: M. Baldauf (2013): A new fast waves solver for the Runge-Kutta dynamical core, COSMO Technical report no. 21 M. Baldauf, S. Brdar (2013): An analytic solution for linear gravity waves in a channel as a test for numerical models using the non-hydrostatic, compressible Euler equations, QJRMS, DOI: 10.1002/qj.2105 M. J. Kurowski, W. W. Grabowski, P. K. Smolarkiewicz (2013): Towards multiscale simulation of moist flows with soundproof equations, JAS, DOI: 10.1175/JAS-D-13-024.1 In preparation: Baldauf, Fuhrer, Kurowski, Piotrowski, Rosa, Vitagliano, Wojcek, Ziemianski (2013): The PP Conservative Dynamical Core, COSMO Technical report ( 7 chapters ready, 1 chapter is still missing)

28 M. Baldauf, U. Blahak (DWD)28 Science plan contributions Main actions planned in a short-term perspective (2015-2017): 1.PP CELO (COSMO-EULAG Operationalization) 2.Further maintenance of the RK dynamical core (‚new fast waves solver‘) 3.Finite volume implicit solver CONSOL 4.Adapt COSMO to run it with extended heights (~ 40 km) 5.Discontinuous Galerkin Euler solver 6.Higher order discretization in the RK scheme 7.Code rewrite by a possible use of a stencil library 8.Improvement of tracer advection schemes. 9.Improvement of 3D diffusion in steep terrain 10.Better upper BC than rigid lid should be found 11.Definition of a COSMO dynamical core test suite 12.Variable time step in the RK scheme for efficiency increase 13.Horizontal grid stretching analogous to the UKMO approach 14. Transition from COSMO-model to a unified ICON-model (~2016)

29 M. Baldauf, U. Blahak (DWD)29 Main actions planned in a long-term perspective (2018-2020): Maintenance of COSMO-EULAG Transition from COSMO-model to a unified ICON-model Introduction of mixed finite volume / spectral methods (e.g. Discontinuous Galerkin or the probably more efficient Continuous Galerkin scheme) Science plan contributions

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