the icon project: development of a unified model using ... · hydrostatic icon model • terrain...
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The ICON project: development The ICON project: development of a unified model using of a unified model using triangular geodesic gridstriangular geodesic grids
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ICON: ICOsahedral grid, Nonhdyrostatic unified (NWP+ climate+chemistry) model• ICON development team:E.Roeckner, D.Majewski, L.B., H. Frank, M.Giorgetta, T.Heinze, L.Kornblueh, P.Ripodas, B.Ritter, W.Sawyer, P.Sanders,U.Schulzweida
•Discussions and/or joint work: N.Botta, F. Giraldo, J.Klemp, R.Klein, D.LeRoux, D.Randall, T.Ringler, H.Tomita
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Outline• Overview of the ICON development project and of the project goals
•Model equations and discretization approach
• Preliminary results of a shallow water model
•Vertical discretization
• Outlook on future work
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Desired features for a new model•Unique framework for large/small scale, lower/upper atmospheric dynamics
•Consistency between conservative discrete tracer advection and continuity equation
•Mass conservative local grid refinementapproach without spurious interface effects: building block for a multiscale model
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Concept of discretization approach•Achieve the same accuracy and efficiency of advanced NWP models…
•…but preserve some discrete equivalents of global invariants relevant to geophysical flow…
•…and narrow the gap with ComputationalFluid Dynamics (CFD) models.
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Nonhydrostatic, compressible flow
[ ] Ru
uηu
u
•−∇=+•∇+∂
∂
Φ∇−∇−−∇=×+∂∂
=•∇+∂∂
)()(
1
0)(
pt
pKt
t
ρερερ
ρρ
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Shallow water flow
0)()(
0)()(
0)(
=•∇+∂
∂
=+∇+×++∂∂
=•∇+∂∂
u
uku
u
cHtcH
Kghft
Hth
ζ
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Geodesic icosahedral grids
•Solve the poleproblem•Special case ofDelaunay triangulation
•Local grid refinement
•Multiscale modelling
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Data structures for grid representation Indirect addressing that preserves data locality
Parallelization: horizontal data decomposition
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Consistent fluxes at coarse/fine interface
dx/8 dx/4Edwards JCP 1996, Bornemann and Deuflhard Num.Math.1996, B. and Rosatti, IJNMF 2002
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Spatial discretization •Finite volume discretization with triangular control volumes: triangular C grid
•Delaunay -Voronoi property
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Spatial discretization, properties
•Vorticity at triangle vertices: discrete Helmholtz decomposition (Nicolaides 1992)
•No spurious vorticity production
•Raviart Thomas reconstruction of velocity, average onto edge for tangential component
xuxu 0 α+=)(
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Discrete shallow water system
llll ghKvftu )()( +−+−=∂∂
νδζ
lil
lli
iCHu
th
,)(
σ∑∈
−=∂∂
lil
lllii
iCHuc
tHc
,)(
)( σ∑∈
−=∂
∂
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Discrete wave dispersion analysis
•Stationary geostrophic solution, no spurious pressure modes
•Two physical gravity wave modes
•Two spurious gravity wave modes: frequencies always higher than physical ones
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Dispersion plot, physical mode
• Less good wavenumber space than quad C
•Zero group velocity at high wavenumbers
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Discrete global invariants
• Mass conservation, consistent discretizations of continuity equation and tracer transport
•Potential vorticity conservation, no spurious vorticity production
•Potential enstrophy conserving variant, energy conserving variant: Sadourny JAS 1975
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Random initial data, f plane
Relative vorticityafter 1000 days integration with random initial data (numerical test carried out by Todd Ringler, CSU)
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Semi-implicit time discretization
lnn
nll
nnl
nl
ghKt
vftuu
)~(
)~(2/12/1
2/12/11
++
+++
+∆−
+∆−=
νδ
ζ
lil
nl
nl
ni
ni
iCHuthh ,
2/11
)(σ∑
∈
++ ∆−=
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Idealized vortex, day 2
Maximum resolution 40 km
Maximum gravity wave Courant number 7
(dt=900 s)
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Rossby Haurwitz wave, day 10
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Flow over a mountain, day 10
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Flow over a mountain:
relative vorticity,
day 10
Colour shading: ICON model results
Black contours: NCAR reference spectral model
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Height field error at day 15
dx≈120 km, dt = 900 s dx≈60 km, dt = 90 s
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Error at day 15, convergence test
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“Shallowness is the greatest vice”
Oscar Wilde
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Options for vertical discretization• Hybrid pressure vertical coordinate + new horizontal discretization: preliminary 3D hydrostatic ICON model
•Terrain following normalized height coordinate + new horizontal discretization: first choice for operational nonhydrostatic model
•Non normalized height coordinate: cut cells (B., JCP 2000, Rosatti and B., Proc. ICFD, 2004)
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Nonhydrostatic coastal modelling
•Results: G.Lang, Bundesanstalt für Wasserbau, Germany
•Numerical model: Casulli and Walters, IJNMF, 2000
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Cut cells + RBF interpolation
Terrain following model (LM) Cut cell nonhydrostatic dynamical core (ARPA Bologna)
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Computational advantages of cut cells
5.12 s26.16 s56.40 sSI Z
11.95 s45.03 s88.95 sSE
COMMtime solver
CPU timesolver
CPU time for 1 hour
21 iter17 iter8 iterSIZ
50 iter21 iter6 iterSI
Residual 0.01% of initial value
Residual 0.1% of initialvalue
Residual 1%of initial value
Simulations run by D.Cesari (ARPA Bologna)
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Future work•Shallow water model on locally refined grids: optimized data structure and parallelization
•Hydrostatic, 3D model on locally refined grids
• Coupling to existing MPI-M/DWD physics packages, impact of spurious modes on simulations with full physics
•Sensitivity of results to local refinement