A 3-D Finite-Volume Nonhydrostatic Icosahedral Model (NIM) Jin Lee.

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Presentation transcript:

A 3-D Finite-Volume Nonhydrostatic Icosahedral Model (NIM) Jin Lee

Earth System Research Laboratory (ESRL) Aeronomy Lab. Climate Diagnostic center Climate Monitoring and Diagnostic Lab Environmental Technology Lab Forecast Systems Lab Chemical Sciences Div Global Monitoring Div Physical Sciences Div Global Systems Div GFDL,NSSL,ARL,AOML,GLERL,PMEL

Earth System Research Laboratory(ESRL) Aeronomy Lab. Climate Diagnostic center Climate Monitoring and Diagnostic Lab Environmental Technology Lab Forecast Systems Lab Chemical Sciences Div Global Monitoring Div Physical Sciences Div Global Systems Div Modeling goal: to develop a non-hydrostatic icosahedral global model for weather and climate applications GFDL,NSSL,ARL,AOML,GLERL,PMEL Director, Dr. A.E. (Sandy) MacDonald

ESRL finite-volume Icos- models (FIM/NIM) FIM (flow-following finite- volume Icosahedral model): Target resolution ≥ 10 km A hydrostatic model consists of 2-D finite-volume SWM coupled with hybrid σ-θ vertical solver. A hydrostatic model for NCEP global model ensemble. NIM (Nonhydrostatic Icosahedral model): Target resolution : O(1 km) and beyond Extension of 2-D finite-volume integration into 3-D integration on control volume defined on the height coordinate. Use the latest GPU technology to speed up high-resolution model calculations. ESMF 19 Apr 20114Global Modeling Program Review

NOAA Earth System Research Laboratory - Boulder, ColoradoPage 5 Finite-volume Integrations on Local Coordinate Novel features of FIM/NIM: 2-D f.-v. operator carried out on straight lines, rather than along the 3-D curved lines on the sphere Lee and MacDonald (MWR, 2009): A Finite-Volume Icosahedral Shallow Water Model on Local Coordinate.

NOAA Earth System Research Laboratory - Boulder, ColoradoPage 6 Finite-volume Integrations on Local Coordinate Conservative and Monotonic Adams-Bashforth 3 rd -order FCT Scheme - Lee, Bleck, and MacDonald (2010, JCP): A Multistep Flux-Corrected Transport Scheme. - Lee, Bleck, and MacDonald (2010, JCP): A Multistep Flux-Corrected Transport Scheme.. Novel features of FIM/NIM:

NOAA Earth System Research Laboratory - Boulder, ColoradoPage 7 Finite-volume Integrations on Local Coordinate Conservative and Monotonic Adams-Bashforth 3rd-order FCT Scheme FIM: Hybrid σ-θ Coordinate w/ GFS Physics - Bleck, Benjamin, Lee and MacDonald (2010, MWR): On the Use of an Arbitrary Lagrangian-Eulerian Vertical Coordinate in Global Atmospheric Modeling.. Novel features of FIM/NIM:

FIM forecasts initialized with GSI initial condition at 00 and 12 UTC (comparisons of FIM and GFS 500 mb ACC) Interpolate GFS initial data to FIM model grid. Perform hydrostatic initialization. Perform 7-day fcst with dx~30km. Same initial condition, terrain & sfc parameters, physics package runing at similar model resolutions (dx~30 km)

Main dropouts from GFS in NH Improvement over GFS from FIM using same initial conditions. 120h NH 500 hPa fcsts -- Nov 2009 – Sept 2010 GFS better FIM better

NOAA Earth System Research Laboratory - Boulder, ColoradoPage 12 Finite-volume Integrations on Local Coordinate Conservative and Monotonic Adams-Bashforth 3rd-order FCT Scheme FIM: Hybrid σ-θ Coordinate w/ GFS Physics Efficient Indirect Addressing Scheme on Irregular Grid - MacDonald, Middlecoff, Henderson, and Lee (2010, IJHPC) : A General Method for Modeling on Irregular Grids. - MacDonald, Middlecoff, Henderson, and Lee (2010, IJHPC) : A General Method for Modeling on Irregular Grids.. Novel features of FIM/NIM:

NOAA Earth System Research Laboratory - Boulder, ColoradoPage 13 Finite-volume Integrations on Local Coordinate Conservative and Monotonic Adams-Bashforth 3rd-order FCT Scheme FIM: Hybrid σ-θ Coordinate w/ GFS Physics Efficient Indirect Addressing Scheme on Irregular Grid Grid Optimization for Efficiency and Accuracy - Wang and Lee (2011, SIAM): Geometric Properties of Icosahedral-Hexagonal Grid on Sphere. Novel features of FIM/NIM:

SBiR SPDN MGCL Comparisons of Icosa-grids UniformityRegularity SBiR MBiR SGCL MGCL

STD SPN MGC Williamson etal.(1992) Case V: Zonal flow over Mountain

SBiR (G8/dt=45 sec)

MGCL (G8/dt=36 sec, blow up with dt=45)

Geostrophic adjustment of finite-volume A-grid model in inviscid and viscid flows

Geostrophic adjustment Experiment : Finite-volume A-Grid SWM : Finite-volume A-Grid SWM  Inviscide model simulation on hexagonal A-grid (dx~60 km) 19

Geostrophic adjustment Experiment : Finite-volume A-Grid SWM : Finite-volume A-Grid SWM  Inviscide model simulation on hexagonal A-grid (dx~60 km) 20

Geostrophic adjustment Experiment : Finite-volume A-Grid SWM : Finite-volume A-Grid SWM  Inviscide model simulation on hexagonal A-grid (dx~60 km) 21

Geostrophic adjustment Experiment : Finite-volume A-Grid Model : Finite-volume A-Grid Model  Inviscide model simulation on hexagonal A-grid (dx~60 km) (  repeat same experiment) 22 typical dissipation operator (small coefficient)

Geostrophic adjustment Experiment : Finite-volume A-Grid Model : Finite-volume A-Grid Model + typical dissipation operator (small coefficient)  Inviscide model simulation on hexagonal A-grid (dx~60 km) 23

Geostrophic adjustment Experiment : Finite-volume A-Grid Model : Finite-volume A-Grid Model + typical dissipation operator (small coefficient)  Inviscide model simulation on hexagonal A-grid (dx~60 km) 24

25 The 2nd-order C-grid scheme over- amplifies mountain waves. Reinecke and Durran (MWR,2009)

NOAA Earth System Research Laboratory - Boulder, ColoradoPage 26 Finite-volume Integrations on Local Coordinate Conservative and Monotonic Adams-Bashforth 3rd-order FCT Scheme FIM: Hybrid σ-θ Coordinate w/ GFS Physics Efficient Indirect Addressing Scheme on Irregular Grid Grid Optimization for Efficiency and Accuracy Novel Features of NIM: - Three-dimensional finite-volume integration. Novel features of FIM/NIM: 3-D control volume box

NOAA Earth System Research Laboratory - Boulder, ColoradoPage 27 Finite-volume Integrations on Local Coordinate Conservative and Monotonic Adams-Bashforth 3rd-order FCT Scheme FIM: Hybrid σ-θ Coordinate w/ GFS Physics Efficient Indirect Addressing Scheme on Irregular Grid Grid Optimization for Efficiency and Accuracy Novel Features of NIM: - Three-dimensional finite-volume integration. - Conservative flux formulation on height coordinate. Novel features of FIM/NIM:

NOAA Earth System Research Laboratory - Boulder, ColoradoPage 28 3-D control volume box Flux form GEs on 3-D control volume on height coord.

NOAA Earth System Research Laboratory - Boulder, ColoradoPage 29 Finite-volume Integrations on Local Coordinate Conservative and Monotonic Adams-Bashforth 3rd-order FCT Scheme FIM: Hybrid σ-θ Coordinate w/ GFS Physics Efficient Indirect Addressing Scheme on Irregular Grid Grid Optimization for Efficiency and Accuracy Novel Features of NIM: - Three-dimensional finite-volume integration. - Conservative flux formulation on z-coordiante. - 3-D volume Integration to calculate PGF. Novel features of FIM/NIM:

NOAA Earth System Research Laboratory - Boulder, ColoradoPage 30 Finite-volume Integrations on Local Coordinate Conservative and Monotonic Adams-Bashforth 3rd-order FCT Scheme FIM: Hybrid σ-θ Coordinate w/ GFS Physics Efficient Indirect Addressing Scheme on Irregular Grid Grid Optimization for Efficiency and Accuracy Novel Features of NIM: - Three-dimensional finite-volume integration. - Conservative flux formulation on z-coordiante. - 3-D volume Integration to calculate PGF. - Horizontal explicit, semi-implicit tri-diagonal solver for vertically propagating acoustic waves. Novel features of FIM/NIM:

NOAA Earth System Research Laboratory - Boulder, ColoradoPage 31 Finite-volume Integrations on Local Coordinate Conservative and Monotonic Adams-Bashforth 3rd-order FCT Scheme FIM: Hybrid σ-θ Coordinate w/ GFS Physics Efficient Indirect Addressing Scheme on Irregular Grid Grid Optimization for Efficiency and Accuracy Novel Features of NIM: - Three-dimensional finite-volume integration. - Conservative flux formulation on z-coordiante. - 3-D volume Integration to calculate PGF. - Horizontal explicit, semi-implicit tri-diag solver for vertically propagating acoustic waves. - Runge-Kutta (RK4) for time discretization Novel features of FIM/NIM:

NOAA Earth System Research Laboratory - Boulder, ColoradoPage 32 Finite-volume Integrations on Local Coordinate Conservative and Monotonic Adams-Bashforth 3rd-order FCT Scheme FIM: Hybrid σ-θ Coordinate w/ GFS Physics Efficient Indirect Addressing Scheme on Irregular Grid Grid Optimization for Efficiency and Accuracy Novel Features of NIM: - Three-dimensional finite-volume integration. - Conservative flux formulation on z-coordiante. - 3-D volume Integration to calculate PGF. - Horizontal explicit, semi-implicit tri-diag solver for vertically propagating acoustic waves. - Runge-Kutta (RK4) for time discretization - Fast GPUs to speed up calculation. Novel features of FIM/NIM:

NIM 2-D test cases: (in 3-D model grid) heat forced circulation, warm bubble, density current (cold bubble), mountain waves, Internal gravity waves (icos-grid) multi-months aqua-planet simulations (icos-grid)

X Y

35 Comparisons of vertical solvers with the warm bubble simulation. A rising thermal in an isentropic atmosphere.

t= 0.0 min Explicit.vs. Implicit tri-diag solvers

t= 14.0 min Explicit.vs. Implicit tri-diag solvers

38 NIM density current simulation. Negative buoyancy to initiate density current.

39 2-D Mountain Waves (DCMIP case 2-1 with h=100 m, dx=500m, a=7km) (Schar etal, 2002, MWR, Klemp 2011, MWR)

Internal Gravity Waves (DCMIP case 3-1, 3-D simulation on icosahedral grid)

41 Same as that of FIM To be used for medium- range weather forecast G lobal/ R egional I ntegrated M odeling s ystem (YSU, Korea) Reference : Hong et al. (APJAS 2012, in review) Climate research high-resolution run * In Namelist, Physics= ‘gfs’ or ‘grims’ Physics packages

NIM 800-day aqua-planet simulation MODEL NIM/GRIMs SST Zonally uniform, max. temp. on equator Resolution G5 (∆x ~ 240 km) Vertical 32 Stretch layers Model top 25 km ∆t 20 min 42 Preliminary Results Zonal Mean SST

Hoskins et al. (1999), Tellus NIM 43 Mean Zonal Wind (3-month)

perturbation pressure meridional wind vertical velocity

MSLP + precip

NIM aqua-planet simulation global precipitation mapNIM precipitation

56 Microphysics sensitivities on model resolutions Microphysics : Reduction of precipitation in WSM3 Resolution : G7 has more precipitation Pick : Large on the equator : Small on mid latitudes G7 G6 G5

Final remarks and future outlook A 3-D f.-v. Nonhydrostatic Icosahedral Model (NIM) dycore has been developed and tested w/ mesoscale benchmarks Incorporated GFS and GRIMs physics packages into NIM dycore. Implemented NIM on GPU and CPU clusters. Aqua-planet simulations to test dynamics/physics interfaces. Test NIM for medium-range NWP at 30-km resolution initialized w/ GSI. Future NIM applications for hurricane track/intensity forecasts and intra-seasonal predictions.