1. Ensemble Post-Processing and it’s Potential Benefits for the Operational Forecaster Michael Erickson and Brian A. Colle School of Marine and Atmospheric Sciences, Stony Brook University, Stony Brook, NY High Ensemble Variability: Hanna 9/6/08 00Z Run 18-42 Hour Acc. Precip

2. NCEP SREF Probability of > 25 mph NCEP SREF Mean SLP and Spread NCEP SREF Mean 500 hPa Height & Vorticity Ensemble Forecasting Tools: What’s Out There Example from 09 UTC 10/25/2010 – 48 Hr Forecast NCEP SREF Probability > 1” Precipitation NCEP SREF Low Pressure PositionsNCEP SREF 500 hPa 5460 m Contour NCEF SREF Probability of > 25 mph NCEP SREF Probability of > 35 mph NCEP SREF Mean 12-hr Snow Sources: http://www.spc.noaa.govexper/sref & http://www.meteo.psu.edu/~gadomski/ewallsref.html/

3. Goals -Evaluate the deterministic and probabilistic biases within the Stony Brook University (SBU) and Short Range Ensemble Forecast (SREF) ensembles. -Apply bias correction and a post-processing technique known as Bayesian Model Averaging (BMA) to the ensembles. -Show how post-processing can be used by operational forecasters and its potential application to river flood forecasting. -Ensembles have biases which can affect both the ensemble mean and probabilistic results. -Can post-processing model data improve both the biases and probabilities derived from the ensemble? Motivation NCEP SREF Temperature Bias > 24 o C No Bias 2X Bias

4. -Analyzed the 00 UTC 13-member Stony Brook University (SBU) and the 21 UTC 21-member Short Range Ensemble Forecast (SREF) system run at NCEP for temperature and precipitation. -Observations consist of the Automated Surface Observing System (ASOS) for temperature and Stage IV rain data for precipitation. -Stage IV data is a blend of rain gauge observations and radar derived rain estimates. -Results are for the 2007-2009 warm seasons (4/1-9/31). Methods and Data Verification Domain Accumulated Stage IV Rain Data Region of Study

5. 10 ETA members at 32 km grid spacing. 5 RSM members at 45 km grid spacing. 3 WRF-NMM members at 40 km grid spacing. 3 WRF-ARW members at 45 km grid spacing. IC's are perturbed using a breeding technique. NCEP SREF 21 Member Ensemble The SBU/SREF Ensemble SBU 13 Member Ensemble 7 MM5 and 6 WRF members run at 12- km grid spacing nested within a 36-km domain. Ensemble uses a variety of initial conditions (GFS, NAM, NOGAPS,and CMC), two cloud microphysical, three convective, and three planetary boundary layer schemes. Region of Study 12-km Model Domain Verification Domain

6. Model Biases 2007-2009 - Temperature Model Bias by Member > 24 o C Diurnal Mean Error Raw Bias > 24 o C for MYJ WRF Member

7. Bias Correction: Cumulative Distribution Function (Hamill and Whitaker 2006) A 50-day training period was used to calculate the cumulative distribution function (CDF) of each model and the observation. The model CDF was then adjusted to the observation over the calibration and validation period value by value. To correct for spatial bias associated with terrain, the bias for each elevation was calculated and removed using a binning approach. CDF For Model and Observation CDF Bias Correction Example

8. Diurnal Root Mean Squared Error Bias Correction 2007-2009 - Temperature Model Bias by Member > 24 o C Diurnal Mean Error Bias Corrected Diurnal RMSE Bias Corrected > 24 o C for MYJ WRF Member Raw Bias > 24 o C for MYJ WRF Member

9. Model Biases 2007-2009 - Precipitation Model Bias by Member > 0.1” Model Bias by Member > 1” Raw Bias > 0.5” for MYJ WRF Member

10. Bias Correction 2007-2009 - Precipitation Model Bias by Member > 0.1” Model Bias by Member > 1” Bias Corrected > 0.5” for MYJ WRF Member

11. -Although biases have been largely corrected, the ensemble is still underdispersed and has unreliable probabilistic forecasts. -Additional post- processing is necessary so that more accurate probabilistic forecasts can be obtained. Reliability for Temp > 24 o C Reliability for Precip > 0.5” Ensemble Underdispersion and Reliability Temp Rank HistogramPrecip Rank Histogram

12. Bayesian Model Averaging (BMA) Bayesian Model Averaging (BMA, Raftery et al. 2005) is designed to improve ensemble forecasts by estimating two things: The weights for each ensemble member (i.e. a “better” member will have more influence on the forecast. The uncertainty associated with each forecast (i.e. a forecast should not be thought of as a point, but as a distribution). Although BMA has been shown to improve ensemble mean forecasts, its main advantage is with probabilistic forecasts. The coldest member is given the greatest weight The second coldest member is given significantly less weight The warmer members have varying weights The BMA derived distribution From Raftery et al. 2005

13. BMA Weights – 2007-2009 Precipitation SREF Member Weights SBU Member Weights

14. Impact of BMA on Reliability after Bias Correction for Warm Season Surface Temperature (2007-2009) Bias Corrected Rank Histogram Reliability > 20 o C BMA Rank Histogram Brier Skill Scores BMA Corrected Bias Corrected -5 0 5 10 15 20 (C)

15. Bias Corrected Rank Histogram Reliability > 0.5” BMA Rank Histogram Brier Skill Scores BMA Corrected Bias Corrected Impact of BMA on Reliability after Bias Correction for Warm Season Surface Temperature (2007-2009)

16. 12 – 36 Hr Accumulated Precipitation Post-Processing Application - 5/17/10 21z NCEP SREF Raw Ensemble Probability > 1.5” Bias Cor. Ensemble Probability > 1.5” BMA Ensemble Probability > 1.5” Stage IV Rain Data BMA Ensemble Probability > 1.5”

17. 6 – 36 hr Accumulated Precipitation Hanna - 9/5/08 21z NCEP SREF Raw Ensemble Probability > 1.5” Bias Cor. Ensemble Probability > 1.5” BMA Ensemble Probability > 1.5” Stage IV Rain Data

18. Tropical Hanna Case: Hydrological Test Case 9/6/08 00z Run: Saddle River: Lodi, NJ QPF from Ensemble Modeled Response: NWS River Forecast System 12 cm 9 cm 6 cm 3 cm 0 cm -33% of members predict major flooding -42% of members predict moderate flooding -58% of members predict flooding Observed Flood Stage ~2.3 m 3.5m 3.0m 2.5m 2.0m 1.5m 1.0m Future work will investigate the potential benefits of BMA for streamflow and flood risk assessment.

19. Conclusions ● Ensemble members suffer from large biases for surface parameters, which can vary temporally, spatially, diurnally and between members. ● The bias correction and BMA improves the probabilistic skill, reliability and dispersion of the Stony Brook + NCEP SREF ensemble. ● Since post-processing improves the ensemble performance spatially, forecasters/users could use BMA for gridded forecast products. ● Although post-processing can remove some systematic biases, it can not correct fundamental problems within the model. For instance, BMA can not correct for large position errors in precipitation forecasts. ● Further development with BMA is needed for extreme weather events such as high QPF forecasts and river flood forecasts given the smaller sample size.