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CAMS GA IFS by Flemming
1. Copernicus
Atmosphere
Monitoring
Service
CAMS General Assembly, Athens, 14-16 June 2016
Anna Agusti Panareda, Samuel Remy, Vincent Huijnen,
J.J-Morcrette, Olaf Stein, Joaquim Arteta, Simon
Chabrillat, Johannes Flemming & Angela Benedetti,
Antje Inness, Sebastien Massart, Richard Engelen as well
as all contributors to IFS and C-IFS
C-IFS: How are
developments integrated
2. 2
IFS : Integrated Forecasting System of ECMWF
A very good NWP forecast and data assimilation model
3. 3
10th anniversary of IFS
1997
IFS : Integrated Forecasting System of ECMWF
A complex model system for forecast and assimilation
4. 4
Adding composition to IFS : Composition -IFS
⢠In GEMS project:
⢠Coupled system IFS-MOZART for chemistry
⢠GHG and aerosol on-line (integrated) in the IFS
⢠MACC I-III: chemistry on-line in IFS
⢠Chemistry - IFS (2009)
⢠Renamed to Composition âIFS: all composition aspects
⢠Composition â IFS : global production system in CAMS
at ECMWF
5. 5
Integration of chemistry & aerosol modules in IFS
Dynamics & Physics
Chemistry
ctm
Dynamics & Physics
Transport &
Chemistry
oasis4
oasis4
oasis4
IFS IFS CTM
Feedback Flow
Coupled System
Feedback: slow
Flexibility: high
Integrated System
Feedback: fast
Flexibility: low
Coupled System
IFS- MOZART3 / TM5
C-IFS
On-line Integration
Flemming et al. 2009
Flexible
but
very un-
efficient
Fast,
consistent
but
higher
coding effort
7. 7
Benefits for CAMS using C-IFS
⢠IFS is the best NWP model on the planet
⢠IFS is a very efficient global model
⢠Operational IFS resolution is currently 9 km globally
⢠CAMS o-suite resolution is 40 km globally
⢠IFS data assimilation (4D-VAR, ENS) used for
composition
⢠Using 4D-Var algorithm (Ensemmble DA)
⢠Infra structure to process assimilated observations
8. 8
Benefits of high resolution model
Mid-tropospheric CH4 [ppb] at 450 hPa
Low resolution FC (80 km, L60) High resolution FC (16 km, L137)
Anna Agusti-Panareda
9. 9
Challenges to use C- IFS for CAMS
⢠Adaptation of data assimilation system to specifics of
composition field and observations
⢠IFS advection does not formally conserve mass
⢠Global mass fixers implemented
⢠Link CAMS development with ongoing IFS development
⢠2-3 new cycles each year
⢠Reproducibility of older cycles
⢠IFS coding standards
10. 10
Towards better integration between C-IFS Components
⢠Between Chemistry, Aerosols and GHG modules
⢠Secondary aerosol formation based on chemistry
⢠Photolysis and surface chemistry modulation by
aerosol
⢠Unified modelling of methane in Chemistry and GHG
⢠Code harmonisation
⢠Composition on NWP (and back !!)
⢠Aerosol in radiation
⢠Ozone in radiation
⢠Land surface and fluxes (emissions and deposition)
16. 16
CAMS
partner
CAMS
ECMWF
IFS team
RD ECMWF
CAMS FD
ECMWF
RD research dep.
FD forecast dep.
e-suite
o-suite
CAMS
VAL
How are C-IFS
developments
integrated ?
Up to 1 year from
development to
o-suite
implementation
18. 18
How are C-IFS developments integrated âŚ
1. Contributing partner (or ECMWF):
⢠Testing (Test A) of individual model development
⢠Delivery to ECMWF/CAMS
2. CAMS-ECMWF Section:
⢠Integrate development in CAMS branch
⢠Testing (Test B) of all integrated model improvements
⢠Submit to ECMWF RD IFS section for ECMWF cycle upgrade
3. ECMWF RD IFS group
⢠Merge new cycle from all ECMWF contributions
4. Forecast Department Copernicus section:
⢠Run experimental CAMS suite (e-suite) and tested by VAL
5. Forecast Department Copernicus section:
⢠Run operational CAMS suite (o-suite)
⢠Each of the steps can take 1-3 month so that it takes up to a year month from model
update to implementation in o-suite
⢠Time line of ECMWF cycle upgrades will be announced to CAMS partners well in
advance