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GODAE OceanView Intercomparison Task Team

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Impact of horizontal resolution is evidenced on kinetic energy levels. ... Most GODAE partners used FTP rather than OPENDAP (not technically efficient) ... – PowerPoint PPT presentation

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Title: GODAE OceanView Intercomparison Task Team


1
GODAE OceanView Intercomparison Task Team
Fabrice Hernandez and Matt Martin
2
Contents
  • Historical background Cal/Val activities during
    GODAE
  • Brief overview of existing metrics definitions
  • Results from final GODAE intercomparison
  • Issues coming out of that intercomparison
  • DISCUSSION
  • Objectives of the Intercomparison Task Team
  • Main areas to focus future effort

3
Historical background 10 years of cal/val
activities in the framework of GODAE
North Atlantic Med
European Seas Global
GODAE
GODAE OceanView
2001
2003
2004
2008
2009
FOAM TOPAZ MFS MERCATOR HYCOM
FOAM TOPAZ MFS MERCATOR DMI-Baltic
FOAM TOPAZ MERCATOR HYCOM MOVE/MRI BLUElinkgt C-NOO
FS
NetCDF COARDS-CF OPENDAP/LAS
NetCDF3
Class 1 ATL Class 2 ATL Class 3 ATL
Class 1 glo Class 2 glo Class 3 glo
Class 1 sea-ice Class 2 sea-ice Class 4 T/S Class
4 sea-ice
Class 1 new Class 2 new
4
GODAE metrics definitions
  • Class 1 daily average model fields interpolated
    onto pre-defined grids (eddy-permitting view) on
    specified levels
  • Class 2 model fields interpolated to
    pre-defined mooring locations and sections.
  • Class 3 transports through sections and other
    integrated quantities such as Meridional
    Overturning Streamfunction and heat transports.
  • Class 4 assessment of forecasting capabilities
    through comparison of model with assimilated and
    independent observations

5
Final GODAE intercomparison
  • Design of the Intercomparison experiment
    (2006-2007)
  • Extending MERSEA Class 1 and Class 2 metrics to
    global scale
  • Definition of intercomparison objectives
  • a) Demonstrate GODAE operational systems in
    operations
  • b) Share expertise and design validation tools
    and metrics endorsed by GODAE operational centers
  • c) Evaluate the overall scientific quality of the
    GODAE operational systems
  • Implementation of metrics computation
  • Demonstration phase 3 month period (Feb, Mar,
    Apr 2008).
  • Phase of synthesis
  • June 2008 to GODAE Final Meeting in Nov. 2008
  • Additional synthesis until January 2009
  • GODAE metrics produced from various groups
    BlueLink, FOAM, HYCOM, Mercator, MOVE/MRI, ...
  • Data put on ftp servers and/or OpenDAP servers.
  • Most of the intercomparison results obtained so
    far have looked at monthly means and standard
    deviations against climatology or some other
    processed data (e.g. SST analyses)
  • No sea-ice results
  • Some intercomparisons (e.g. done by the
    Australians) have focussed more on comparison
    with assimilated and independent observations,
    e.g. SST, SLA, Argo and surface drifters, in the
    Indian Ocean and South Pacific regions.

6
GODAE systems in comparison
Mercator NEMO ECMWF SEEK RkF T,S, SLA, SST
HYCOM HYCOM FNOC-NOGAPS NCODA MvOI T,S,(SLA), SST, ice
FOAM NEMO UK-Met T, S, SLA, SST, ice
BLUElink ind/spa MOM4 BoM BODAS EnOI T,S,SLA,TG, SST
TOPAZ nat/arc HYCOM ECMWF EN-kF T,S, SLAmaps, SST, ice
MOVE/MRI npa MOVE JMA MRI - 3Dvar T,S, SLA, MG-SST
C-NOOFS nw-nat NEMO Env. Canada no
7
HYCOM
Mercator
FOAM
8
Intercomparison in the TAT
Snapshot SST comparison the 15th of February 2008
with respect to OSTIA. Numbers in brackets
correspond to RMS differences in the box limited
area in the Gulf of Guinée (15W-5E and
5S-5N), and the box limited area for the
Northern Tropical Atlantic (55-15W and 5-25N),
plotted for the OSTIA figure. Units 3/-3 in
Kelvin.
0.35
0.41
HYCOM (0.73 / 0.35)
0.73
0.30
0.50
0.39
PSY2V3 (0.34 / 0.39)
0.34
0.41
9
Box averaged SST
0.5C
0.5C
10
Assessment of EKE in NAT
TOPAZ
C-NOOFS
FOAM
SURCOUF
HYCOM
Mercator
11
Monthly comparison in April08
12
(No Transcript)
13
Final GODAE intercomparison general scientific
outcomes
  • GODAE eddy-permitting systems are consistent
    (i.e. match qualitatively the climatology,
    general patterns of the ocean circulation) and
    there is no bad surprise
  • Accuracy assessment reveals differences, biases,
    possible errors in model or assimilation schemes
    These evidence are a first step for targeted
    corrections and improvements
  • Impact of horizontal resolution is evidenced on
    kinetic energy levels.
  • Further work need to be done to identify the
    causes of differences between the systems (e.g.,
    impact of forcing, data assimilation schemes.)

14
Final GODAE intercomparison
  • Successes of the intercomparison
  • The hindcasts/forecasts were made available and
    easily accessible (and people were responsive if
    there were problems accessing the data).
  • Most/all of the work was done using the Class 1
    fields. These fields were generally produced
    using the agreed definitions (at least close
    enough to make it relatively easy to use them).
  • The comparison of the Class 1 fields highlighted
    some interesting differences between the systems.
  • Visibility of this work through scientific
    communication and publication
  • Observations were made available by the observing
    community, involved now in operational
    oceanography, and supporting the ocean
    forecasting centers

15
Final GODAE intercomparison
  • Shortcomings of the intercomparison
  • Some systems produced the metrics in their normal
    operational setting, whereas others were re-run
    in hindcast mode.
  • Some groups upgrade their systems in the meantime
    of the Intercomparison synthesis
  • Some systems produced forecasts and others just
    analysis fields.
  • Class 1 still need some homogenisation
  • Class 2 and 3 metrics were produced by some
    systems but not all, and no comprehensive
    assessment of them was carried out.
  • Very little/no work done on Class 4 metrics
    intercomparison
  • Most GODAE partners used FTP rather than OPENDAP
    (not technically efficient)
  • A demonstration rather than a routine
    intercomparison.
  • A three month period is a really short period of
    time to overview ocean forecasting system
    behaviour and performance
  • It would have been useful to meet to present and
    discuss results the calendar was very tight
  • Several groups had problems to fully contribute
    to the exercise, and human resources dedicated to
    intercomparison synthesis were not available in
    all forecasting centres.

16
Discussion and outlook
  • What is the role of a validation/intercomparison
    Task Team?
  • Strategy of the validation/intercomparison Task
    Team
  • Clarify workplan of Intercomp/Val TT and
    interactions with
  • OSE/OSSE TT
  • Coastal and Shelf Seas TT
  • Biogeochemical TT
  • ET-OOFS
  • WCRP-CAS WGNE

17
1. What is the role of a validation/intercompariso
n Task Team?
  • Core scientific activity develop metrics, share
    experience, evidence differences,
    cross-fertilized ideas among GODAE centers
  • Be consistent as a group in our monitoring
    policy provide tool for monitoring routinely the
    systems, and controlling inputs (e.g. link with
    data providers), and outputs (mandatory link with
    users)
  • Main benefit improvements of the systems, and
    the quality of products
  • Provide visibility as GODAE community
    demonstration, publications

18
2. Strategy of the validation/intercomparison
Task Team
  • Rely on new targeted intercomparison exercices ?
  • Establish permanent monitoring among the OOFS?
  • Expect outcomes from regional activities (e.g.
    MyOcean, US Navy)?

19
2. Strategy of the validation/intercomparison
Task Team Suggested scientific aspects that
should be addressed
  • Extend comparison with other set of independent
    observations, e.g. ocean colour, surface drifters
  • Assessing the performance of the data
    assimilation using observation-minus-background
    and observation-minus-analysis statistics
  • Useful to show accuracy of short-range forecasts
    and the performance of the assimilation.
  • Different analysis time-windows and operational
    schedules make it difficult to intercompare (o-b)
    between systems.
  • Assessing the performance of the model through
    estimates of forecast skill
  • Anomaly correlations and RMS differences between
    forecasts and analyses (and between forecasts and
    observations).
  • Multi-model ensemble statistics
  • provide error levels and monitoring tools
  • Design user oriented metrics for targeted
    applications (ocean climate monitoring, oil
    spill, SR)
  • Demonstration of routine validation activity

Internal
External
20
3. Clarify workplan of Intercomp/Val TT and
interactions
  • Take into account new OOFS (NCEP, MFS, China)
  • Diagnostics that allow the characterisation of
    biases, long term changes (link with GSOP)
  • Link with coastal validation
  • Assessing the accuracy/impact of IC/BC
    (downscaling)
  • Share scientific assessment methodology
  • Link with biogeochemistry validation
  • Assessing the accuracy/impact of the physical
    variables (vertical diffusion, coupling)
  • Share scientific assessment methodology
  • Link with OSE/OSSE TT (characterize the impact of
    incoming data, feedbacks to relevant data
    providers)
  • Develop common metrics for both validation and
    data impact assessment

21
Suggested plan for the coming months
  • Use of existing Feb-Mar-April 2008 dataset
  • Extended scientific validation ?
  • Inform which metrics should be integrating a
    possible routine monitoring (daily NRT
    production)
  • Discuss future implementation depending on chosen
    strategy
  • Prepare workplan roadmap document
  • By end of september 2009
  • Review by OOFS
  • Beginning of implementation in 2010
  • Prepare calendar for meetings/discussions
  • Topics to be addressed in the roadmap
  • Discuss technical aspect of NRT production
    (storage and exchange) possible link with
    ET-OOFS
  • focus on a sub-set of useful metrics
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