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Recent Status of NEMS/NMMB-AQ Development

Recent Status of NEMS/NMMB-AQ Development. Youhua Tang 1 , Jeffery T. McQueen 2 , Sarah Lu 1 , Thomas L. Black 2 , Zavisa Janjic 2 , Mark D. Iredell 2 , Carlos Pérez García-Pando 3 , Oriol Jorba Casellas 3 , Pius Lee 4 , Daewon Byun 4 , Paula M. Davidson 5 , and Ivanka Stajner 6

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Recent Status of NEMS/NMMB-AQ Development

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  1. Recent Status of NEMS/NMMB-AQ Development Youhua Tang1, Jeffery T. McQueen2, Sarah Lu1, Thomas L. Black2, Zavisa Janjic2, Mark D. Iredell2, Carlos Pérez García-Pando3, Oriol Jorba Casellas3, Pius Lee4, Daewon Byun4, Paula M. Davidson5, and Ivanka Stajner6 1. Scientific Applications International Corporation 2. NOAA/NCEP/EMC 3. Barcelona Supercomputing Center, Edificio Nexus II c/ Jordi Girona 29, Barcelona, Spain 4. NOAA Air Resource Laboratory 5. Office of Science and Technology,NOAA/National Weather Service 6. Noblis Inc, Falls Church, VA

  2. An inline model allows frequent interaction between meteorological and air quality processes. - Especially important for non-hydrostatic scales when meteorological features have fine temporal and spatial scales. This air quality model can be driven by different meteorological models (which can be on different grids, e.g. for quick testing) A common framework allows varying degrees of coupling and flexibility. Advantages of the ESMF Framework for Air Quality Application

  3. Pros and Cons of the Inline Model • Immediate and fast data access to the corresponding meteorological model. • Overall efficiency by reducing the intermediate I/O files • Can provide in-situ feedback to the met model • Depends more on the met model than the offline version. • Could slow down the meteorological forecast when running in the same domain

  4. NOAAEnvironmental Modeling System (NEMS)(uses standard ESMF compliant software) Application Driver ESMF Superstructure (component definitions, “mpi” communications, etc) Analysis -------------- Ocean ------------- Wind Waves -------------- LSM -------------- Ens. Gen. -------------- Other Atmospheric Model Dynamics (1,2) Physics (1,2,3) Coupler1 Coupler2 Coupler3 Coupler4 Coupler5 Coupler6 Etc. Chemistry 1-1 1-2 1-3 2-1 2-2 2-3 Multi-component ensemble + Stochastic forcing Bias Corrector Post processor & Product Generator Verification Resolution change ESMF Utilities (clock, error handling, etc) * Earth System Modeling Framework (NCAR/CISL, NASA/GMAO, Navy (NRL), NCEP/EMC), NOAA/GFDL 2, 3 etc: NCEP supported thru NUOPC, NASA, NCAR or NOAA institutional commitments Components are: Dynamics (spectral, FV, NMM, FIM, ARW, FISL, COAMPS…)/Physics (GFS, NRL, NCAR, GMAO, ESRL…)

  5. NEMS Atmosphere Component class Color Key Coupler class Atmospheric Model Completed Instance Under Development unified atmosphere including digital filter Future Development Dynamics Physics and Chemistry Dyn-Phy Coupler ARW NMM-B NAM Phy CMAQ Chemistry Simple FVCORE Spectral GFS Phy Regrid, Redist, Chgvar, Avg, etc GOCART Aerosol model NOGAPS FIM WRF Phy COAMPS FISL Navy Phy Simple Chemistry NMM-B: Nonhydrostatic Multiscale Model on B grid FIM: Flow-following finite-volume Icosahedral Model FISL: Fully-Implicit Semi-Lagrangian FVCORE: Finite-Volume Dynamical Core NOGAPS: Navy's Operational Global Atmospheric Prediction System COAMPS: Coupled Ocean/Atmosphere Mesoscale Prediction System

  6. Two Inline Methods A) Air Quality Model Dynamics Physics Chemistry Meteorological Model Dynamics Physics Exchange data via the memory with specified time frequency Meteorological I/O AQ I/O B) Meteorological Model/Air Quality Model Dynamics with passive tracers Physics with AQ species Chemistry Unified I/O

  7. Pros and Cons of the two Methodsin NEMS • Method A: Allows flexibility and can be made consistent • Can keep most of the original AQM architecture with minimal changes. • Different components can run on different grids supported by ESMF • Inconsistencies may exist between meteorological and air quality models • Overhead due to different dynamics/physics and diagnostic variables • Method B: Focuses on efficiency and is inherently consistent • All computation uses common native grid and dynamics • High efficiency • Low flexibility. Introduces dependency on certain meteorological dynamics or physics components • Require positive-definite mass-consistent advection scheme and inclusion of AQ • processes in the meteorological modules

  8. Import State Export State Import State Export State PHYSICS Gridded Component INIT-RUN-FINALIZE Input Emissions Input Dry Depositions PBL Mixing (MYJ) Photolysis Calculation Chemical Reactions Convective Mixing Wet/Cloud Scavenging DYNAMICS Gridded Component INIT-RUN-FINALIZE Chemical Initialization Lateral Boundary Conditions Chemical Advection Chemical Output MAIN Program Framework of NEMS/NMMB-AQ Import State Export State Method B MAIN Gridded Component INIT-RUN-FINALIZE Import State Export State Dyn-Phys COUPLER Component INIT-RUN-FINALIZE Import State Export State Import State Export State General Output Gridded Component INIT-RUN-FINALIZE General Output Gridded Component INIT-RUN-FINALIZE

  9. NMM-B Dynamical Core • Coordinate System and Grid • Global lat-lon, regular grid • Regional rotated lat-lon, more uniform grid size • Arakawa B grid (in contrast to the WRF-NMM E grid) • Pressure-sigma hybrid(Sangster 1960; Arakawa and Lamb 1977; Simmons and Burridge 1981) • Flat coordinate surfaces at high altitudes where sigma problems worst (e.g. Simmons and Burridge, 1981) • Higher vertical resolution over elevated terrain • No discontinuities and internal boundary conditions • Lorenz vertical grid • NMM-B Advection Scheme for Passive Tracers • Conservation through flux cancelations, not forced a posteriori • Quadratic conservative advection scheme coupled with continuity equation • Crank-Nicholson for vertical advection • Modified Adams-Bashforth for horizontal advection • Advection of square roots of tracers (c.f. Schneider, MWR 1984) provides positive definiteness • Quadratic conservation provides tracer mass conservation • Monotonization with a posteriori forcedconservation to correct oversteepening

  10. The NMM-B’s new scheme is shown to be mass conservative

  11. Courtesy: Barcelona Supercomputing Center (BSC) Designated center within WMO Sand and Dust Storm Warning Advisory and Assessment System (SDS-WAS), NMM/BSC-DUST model

  12. NMMB Dry Run ONLY without convective mixing or wet scavenging

  13. Solutions to avoid slowing down the Met forecast • Run AQM on sub-domains • Run AQM as a separate cycle from the operational Met model

  14. Summary • The development of NEMS/NMMB inline air quality model has started using ESMF framework • Most of related chemical/physical modules are zero-dimensional or one dimensional, which can be placed into this system directly, either as normal subroutines or as an ESMF gridded component. We will use CMAQ existing chemical modules in this system. • The new mass-conservative NMM-B advection scheme can support air quality applications.

  15. Next steps for NEMS/NMMB-AQ development • Add convective mixing for passive tracers • Add in-cloud and under-cloud chemical scavenging. • Replace interpolated emissions with native- grid emissions (CMAQ SMOKE package) • Biogenic emission and Dry deposition inline • Alternative more flexible coupling approach through a separate chemistry grid component (method A) will be explored • Feedback case testing – leverage NEMS radiative interactions

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