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Recent changes in the NCEP global ensemble forecast system. Yuejian Zhu, Zoltan Toth, Richard Wobus*, and Lacey Holland* EMC/NCEP *SAIC at NCEP September 19 2003 http://wwwt.emc.ncep.noaa.gov/gmb/ens/ Acknowledgements: H.-L. Pan, S. Lord, D. Michaud, and T. Marchok. Contents. - PowerPoint PPT Presentation
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Recent changes in the NCEP global ensemble forecast system
Yuejian Zhu, Zoltan Toth, Richard Wobus*, and Lacey Holland*
EMC/NCEP*SAIC at NCEP
September 19 2003http://wwwt.emc.ncep.noaa.gov/gmb/ens/
Acknowledgements:H.-L. Pan, S. Lord, D. Michaud, and T. Marchok
Contents
Introduction Configuration of NCEP global ensemble
forecast system Recent implementation (May 2003) Performance statistics Next implementation (Oct-Nov. 2003) Ongoing research / Plans
Introduction
NCEP global ensemble system operated daily since December 1992.
Initial perturbations are generated by Breeding method (Toth and Kalnay, 1993 1997)
Ensemble size: <10 --> 25 (now) 45 (next month)
Ensemble resolution: T62 T126 (first 180 hours)
Ensemble based products have been generated. Wide range of users both nationally and
internationally Evaluation (including potential economic value)
NCEP global ensemble current configuration
High resolution Control 4 cycles (00, 06, 12, 18
UTC) 3 different resolutions
(from high to low) Ensemble
2 cycles (00, 12 UTC) 2 different resolutions 5 pairs (+/-
perturbation) BGM
Total 1 low resolution control 25 global forecasts/day
Recent implementation (April 29 2003)
Motivation: Bring initial perturbation amplitude more in line with actual uncertainty in analysis
Compare fit of first guess to observational data with perturbation amplitude
Additional consideration: NCEP global ensemble does not account for model error
Set initial amplitudes somewhat above level of initial uncertainty (forecast error at 2-3 days matches ensemble pert. amplitudes)
Change: Revise mask used to set perturbation amplitudes: 10% reduced for NH 60% reduced for SH 50% reduced for tropics
Experimental period: 20020824 – 20020930 (38 days)
Results: 1.5% (NH) and 7.6% (SH) RMS error reduction
Experimental results (1)
NH 500hPa height Brier Skill Scores (BSS) and decomposition (resolution and reliability)
No significant impact by reducing spread by 10%
Similar results for PAC, RMS, and other probabilistic scores
--- operational (control)--- I – reduced spread--- J – reduced spread
Experimental results (2)
Top: SH 500hPa height PAC
There is a significant improvement from short to medium range
Bottom: SH 500hPa height RMS errors
Similar to PAC, reduced spread, decreased RMS errors
--- operational (control)--- I – reduced spread--- J – reduced spread
--- Climate mean forecast
spread
Experimental results (3)
Top: SH 500hPa height economic values for 10:1 cost-loss ratio
Experiments have higher values for all lead times
Bottom: SH 500hPa height ROC area skill scores (ROCASS)
Experiments improve probabilistic forecast skill
Experimental results (4)
Tropical storm track errors
Atlantic, east Pacific and west Pacific regions
Comparing to operational ensemble, ensemble control and GFS
Current performance (1)
45-day statistics Top: NH (20-80N) 500hPa
height PAC for GFS, ensemble control and mean, ensemble mean is better than GFS for 4-day and beyond
Bottom: NH 500hPa height RMS for GFS, CTL, ensemble mean and climate, and ensemble spread
Current performance (2)
45-day statistics Top: SH (20-80S) 500hPa
height PAC for GFS, ensemble control and mean, ensemble mean is better than GFS for 1% for 5-day forecast
Bottom: SH 500hPa height RMS for GFS,CTL, ensemble mean and climate, and ensemble spread
Next implementation
Time: October-November 2003 Extending T126 model resolution from 84
hours to 180 hours Increasing ensemble size from 25 to 45 by
adding 10 (5 pairs) at 0600UTC and 10 (5 pairs) at 1800UTC
Adding more probabilistic forecast products: PQPF (old, total precipitation), PQRF(rain), PQSF(snow), PQIF(ice pellets) and PQFF(freezing rain)
Ongoing work
Adapt ETKF for rescaling in (place of) breeding method (Wang and Bishop)
Explore new ways to account for model related errors in ensemble forecasting (use different/modified convective schemes, etc)
Bias-correct first and second moments of ensemble
Plans Develop North American Ensemble Forecast System
(Joint work with Meteorological Service of Canada, for joint NCEP-MSC ensemble products)
Inter-compare 4 different ensemble-based data assimilation algorithms (collaborative work among 4 groups)