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CTM IFS interfaces GEMS GRG

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Orography & surface pressure. CTMs should use an orography consistent with the spectral truncation of the IFS output ... Different resolution and orography ... – PowerPoint PPT presentation

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Title: CTM IFS interfaces GEMS GRG


1
CTM - IFS interfacesGEMS- GRG
  • Review of meeting in January and more recent
    thoughts
  • Johannes Flemming

2
Background
  • Assimilating remotely sensed observation about
    atmospheric composition
  • GEMS production is hosted at ECMWF
  • Integrated Forecast System (IFS) provides
    background
  • Transport, emissions, deposition and chemical
    conversion
  • GRG-specific problem
  • Chemical mechanism with gt 40 species can hardly
    be incorporated in IFS

3
GRG - approach
  • Include observable species in IFS (transport and
    assimilation)
  • O3, NO2, SO2, CO and HCHO can be observed from
    space (?)
  • Assimilate species in IFS with ECMWF 4D-VAR
  • Simulated source and sinks by coupling Chemical
    Transport Models (CTM)
  • CTM MOZART (MPI-H), TM5 (KNMI), Mocage
    (meteo-france)

4
What do we have to consider?
  • Fields to be exchanged
  • Choice of coupling method
  • Choice of model grid
  • Frequency and timing of exchange in forecast and
    assimilation runs
  • Common computing environment for IFS and CTMs
  • Harmonised interfaces

5
Coupling method
  • Coupler OASIS4
  • Is being developed in PRISM (work in progress)
  • Can exchange 3D fields between different grids
  • Mass conservation atmospheric balances (?)
  • Support of reduced Gaussian grid (?)
  • Spectral and grid point presentation
  • Coupling on the level of the MPI processes
  • CTM should be MPI parallel
  • File output possible
  • Coding interfaces and control by XML scripts
  • GEMS needs will be considered in development

6
CTM IFS
  • Horizontal resolution
  • IFS reduced Gaussian grid, T159
  • CTM Regular or Gaussian grid, T63/ T42
  • Vertical resolution
  • IFS L90 Levels in sigma hybrid coordinate
  • CTM L20-30 Levels in sigma hybrid coordinate
    (same coefficients)
  • Orography surface pressure
  • CTMs should use an orography consistent with the
    spectral truncation of the IFS output
  • Advection scheme, chemical mechanism
  • MPI parallelisation (?)

7
IFS fields to CTM
  • Wind components mass fluxes
  • Temperature
  • Humidity
  • Clouds
  • Convective mass fluxes
  • Profiles of precipitation
  • Vertical diffusion coefficient
  • IFS concentrations (data assimilation mode)
  • Surface pressure
  • ?

8
CTM fields to IFS
  • Production P
  • Loss rate L
  • LC and PC due to chemistry (3D)
  • PE due to emissions (2D)
  • LD due to deposition (2D/3D cloud)
  • Not standard output
  • LC , PC ,LD and PE are not independent
  • Totals only (?)
  • Concentrations (Initial conditions) (?)

9
Dislocation problem
10
Dislocation problem
  • IFS concentration fields differ from CTM fields
    because of different transport and data
    assimilation
  • CTMs PL is not consistent with IFS
    concentration fields
  • IFS chemical analysis is not chemically
    consistent with CTM fields (difficult to merge)
  • Is this an issue ?

11
Forecast mode
  • 2-way coupling requires synchronous run
  • Exchanged met-data and PL have to be assumed
    constant till next coupling
  • PL IC required
  • How to consistently merge IFS chemical analysis
    in CTM IC
  • 1-way coupling (CTM gets met-data)
  • would allow lagged coupling (temporal
    interpolation of met-data)

12
Coupling in Forecast mode
13
ECMWF 4D-VAR Data assimilation T,u,v,q,O3
O3 transport chemistry
O3 advection only
O3 transport chemistry
14
Coupling in Data assimilation mode
  • Tangent linear and adjoint of coupled system
    (IFS-OASIS4-CTM) would be needed (not feasible)
  • Problems
  • Including PL chemistry in inner loops (Do we
    need it? What are the consequences?)
  • How to consistently transfer assimilated
    concentration to CTM IC
  • Impact of analysed met data on CTM (PL)
  • 1. Option
  • No chemistry in 4D-VAR inner loops (as currently
    for Ozone)
  • 2. Option
  • Fixed L and P terms from CTM forecast
  • no impact on CTM except for met data in out loop
  • Does coupler work in 4DVAR (?)

15
CTM-implementation
  • GEMS partners access to ECMWF HPCF
  • Member state or special project access
  • Source code management for CTM and Coupler
  • Perforce projects for CTMS and OASIS (license?)
  • Build and scheduling system for CTMs and Coupler
  • ECMWF build-system for the CTMs
  • Code sharing CTM and IFS
  • no restriction to the CTM code (?)
  • CTM parallelisation
  • The CTMs need to be MPI-parallel for efficient
    coupling
  • OASIS MPI1 mode only on IBM
  • Model have to run with communicator provided by
    coupler
  • Seems to be no problem

16
Status and (short-term) Plans at ECMWF
  • IFS code
  • CY29r2 based version with 5 GRG prognostic and
    Aerosol
  • Identify best position for OASIS4 interfaces (met
    and chemistry)
  • Routine for global budget calculation
  • OASIS4 coupler
  • Playing with code and toy models (local linux
    environment)
  • No support of reduced Gaussian grid
  • MPI2 mode (spawning) not possible
  • Graphical Interface ready for editing of XML
    configuration files
  • Build CTM toy model and couple it to IFS
  • CTM Implementation
  • Meeting on technical issues
  • TM5 and Mozart run at ECMWF HPCF in special
    project status
  • Implement CTMs in GEMS environment as soon as
    code is available

17
Issues CTM-IFS coupling I
  • Technical implementation of coupler
  • How long will it take to get OASIS4 running with
    IFS and CTM
  • CTM efficiency, MPI communication, Coupler
    efficiency
  • Data to be exchanged
  • List complete
  • Grids support (vertical and horizontally)
  • Spectral or Grid point
  • Different resolution and orography
  • Mass conservative interpolation
  • Coupling frequency
  • High temporal coupling frequency reduces problems
    (requires efficient coupler)

18
Issues CTM-IFS coupling II
  • Constant LP and met-data assumption
  • Careful analysis of temporal scales of P and L
  • Coupling in data assimilation mode
  • chemistry modelling in inner loops
  • Analysed met-data for CTM
  • Different resolution and orography
  • Different concentration patterns in CTM and IFS
    (Dislocation problem)
  • PL fields dislocated
  • Chemically consistent CTM analysis
  • More chemistry in IFS (?)
  • Using more balanced tracers (NOx, Ox) in IFS

19
END
  • Thank You!
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