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SPC Ensemble Applications:SPC Ensemble Applications:Current Status, Recent Developments, Current Status, Recent Developments,
and Future Plansand Future Plans
David Bright
Storm Prediction CenterScience Support Branch
Norman, OK
4th Ensemble User WorkshopTuesday, 13 May 2008
Laurel, MDWhere Americas Climate and Weather Services Begin
Outline: SPC Ensemble Applications
• Current Status– Large-Scale Predictability: GEFS and NAEFS– Mesoscale Guidance: SREF
• Recent Developments– HWT/Spring Experiment Storm-Scale
Ensemble Forecst (SSEF)– Rapid-Refresh Ensemble Forecast
• Ongoing and Future Plans
Application of the GEFS and NAEFS
Day 4 through 8: Severe Weather Outlook Day 3 through 8: Fire Weather Outlook
• Assess the large-scale pattern and its predictability• Anticipate the spectrum of possible high-impact weather• Three Forecast categories:
1) Potential Too Low2) Predictability Too Low3) Outlook An Area
168h Forecast Valid 00 UTC 22 Oct 2007
GEFS Ensemble Mean: 500 mb Height and Vorticity
Application of the GEFSGEFS in NMAP2: Pattern
168h Forecast Valid 00 UTC 22 Oct 2007
GEFS Ensemble Spaghetti: 500 mb Height (Single contour at 5760 m)
Application of the GEFSGEFS in NMAP2: Predictability and spread
168h Forecast Valid 00 UTC 22 Oct 2007
GEFS Ensemble: Mean 500 mb Height and its Departure from Normal (# of SD)
Application of the GEFSGEFS in NMAP2: Departure from normal
168h Forecast Valid 00 UTC 22 Oct 2007
NAEFS Ensemble: 500 mb Mean Height and its Standard Deviation
Application of the NAEFS
NAEFS via WEB: Predictability of the large-scale pattern
Mesoscale Scale
• 90% of products here…so most work in this area
• Build confidence
• Assess range of plausible solutions
Application of the SREF Ensemble • The High Impact Challenge: High impact events often occur on time and space scales below the resolvable resolution of most observing, forecasting (and ensemble) systems
• Key Application Premise: We use knowledge of the environment, unresolved processes, and consider uncertainty, to determine the spectrum of possible hazardous weather, when and where it may occur, and how it may evolve over time
Applications of Mesoscale Applications of Mesoscale Ensemble Guidance at the SPCEnsemble Guidance at the SPC
• Develop specialized guidance for the specific application (severe weather, fire weather, winter weather)
• Design guidance that…– Helps blend deterministic and ensemble approaches– Provide guidance for uncertainty/probabilistic forecasts– Provide guidance that aids (deterministic) confidence– Illustrates a range of plausible scenarios– Allows for diagnostic analysis – is not just a statistical black-box– Probabilities and joint probabilities most commonly applied
SREF Probability of STP Ingredients: Time Trends
48 hr SREF Forecast Valid 21 UTC 7 April 2006
Prob (MLCAPE > 1000 Jkg-1)
X
Prob (6 km Shear > 40 kt)
X
Prob (0-1 km SRH > 100 m2s-2)
X
Prob (MLLCL < 1000 m)
X
Prob (3h conv. Pcpn > 0.01 in)
Shaded Area Prob > 5%
Max 40%
SREF Probability of STP Ingredients: Time Trends
36 hr SREF Forecast Valid 21 UTC 7 April 2006
Prob (MLCAPE > 1000 Jkg-1)
X
Prob (6 km Shear > 40 kt)
X
Prob (0-1 km SRH > 100 m2s-2)
X
Prob (MLLCL < 1000 m)
X
Prob (3h conv. Pcpn > 0.01 in)
Shaded Area Prob > 5%
Max 50%
SREF Probability of STP Ingredients: Time Trends
24 hr SREF Forecast Valid 21 UTC 7 April 2006
Prob (MLCAPE > 1000 Jkg-1)
X
Prob (6 km Shear > 40 kt)
X
Prob (0-1 km SRH > 100 m2s-2)
X
Prob (MLLCL < 1000 m)
X
Prob (3h conv. Pcpn > 0.01 in)
Shaded Area Prob > 5%
Max 50%
SREF Probability of STP Ingredients: Time Trends
12 hr SREF Forecast Valid 21 UTC 7 April 2006
Prob (MLCAPE > 1000 Jkg-1)
X
Prob (6 km Shear > 40 kt)
X
Prob (0-1 km SRH > 100 m2s-2)
X
Prob (MLLCL < 1000 m)
X
Prob (3h conv. Pcpn > 0.01 in)
Shaded Area Prob > 5%
Max 50%
Severe Event of April 7, 2006• SREF severe weather fields increased forecaster
confidence resulting in a “High Risk” outlook• First ever Day 2 outlook High Risk issued by SPC • More than 800 total severe reports
– 3 killer tornadoes and 10 deaths
http://www.spc.noaa.gov/exper/sref/
SPC SREF Webpage for Mesoscale High-Impact Applications
http://w1.spc.woc.noaa.gov/exper/sref/frames.php?run=case_2007060703
Case study support added for WFOs
http://www.spc.noaa.gov/exper/sref/
SPC SREF Webpage for Mesoscale Applications is Popular
SPC SREF Webpage for Mesoscale Applications: Plumes
Click on forecast hour for dSREF/dt depiction(Courtesy of Steve Listema and Steven Zubrick, WFO Sterling)
SPC SREF Webpage for Mesoscale Applications: dSREF/dt
SPC SREF Webpage for Mesoscale Applications: dSREF/dt
• Decomposition of severe:– Probability of > 1 tornado
• Improved calibrated thunderstorm
• Rapid Refresh Ensemble System (RREF)– Based on time-lagged RUC– Guidance for convective initiation (and initial
operational storm scale ensembles will likely require scaled time lagging
Recent SREF Developments and Plans
RREF: Calibrated Hourly Thunderstorm Probability
RREF: Calibrated Hourly Thunderstorm Probability
Storm Scale
Future Applications: Explicit High Impact Ensembles
• NOAA Hazardous Weather Testbed (HWT)• HWT Spring Experiment
Focused on experimental high-res WRF forecasts since 2004 (dx ~2-4 km)• Convection allowing ensemble forecasts (2007-2009) to address uncertainty
10 WRF members 4 km grid length over 3/4 CONUS Major contributions from: SPC, NSSL, OU/CAPS, EMC, NCAR
• Evaluate the ability of convection allowing ensembles to predict: Convective mode (i.e., type of severe wx) Magnitude of severe type (e.g., peak wind) Aviation impacts (e.g., convective lines/tops) QPF/Excessive precipitation Year 1 Objective (2007): Assess the role of physics vs. initial condition uncertainty at high resolution
2003 Spring Experiment
2 km AGL
5 km AGL
Convective Mode: Supercell DetectionBesides simulated reflectivity, need a quantitative tool for supercell detection
and strength in deterministic and ensemble forecasts
Probability Updraft Helicity > 50 m2/s2
Supercell Detection
F026: Valid 02 UTC 22 Apr 2008UH > 50 + 25 mi
Probability Updraft Helicity > 50 m2/s2
Radar BREF 0142 UTC 22 Apr 2008
Probability Updraft Helicity > 50 m2/s2
View of the left split looking south from Norman, OK (0145 UTC 22 Apr 2008)
(Numerous large hail reports up to 2.25”)
Jack Hales
Convective Mode: Linear Detection
• Determine contiguous areas exceeding 35 dbZ
• Estimate mean length-to-width ratio of the contiguous area; search for ratios > 5:1
• Flag grid point if the length exceeds:– 50 miles– 100 miles– 200 miles
Probability Linear Mode Exceeding 200 miles
Squall Line Detection F024: Valid 00 UTC 18 Apr 2008Linear mode + 25 miles
Probability Linear Mode Exceeding 200 miles
Squall Line Detection F026: Valid 02 UTC 18 Apr 2008Linear mode + 25 miles
Squall Line Detection
Probability Linear Mode Exceeding 200 miles
F028: Valid 04 UTC 18 Apr 2008Linear mode + 25 miles
Base Reflectivity 0140 UTC 18 April 2008
Radar Reflectivity Valid 02 UTC 15 May 2007
Linear Convective Mode: Impacts
Direct Severe Guidance from SSEFProbability of Severe Thunderstorms based on “synthetic reports”
Direct Severe Guidance from SSEFProbability of Severe Thunderstorms based on “synthetic reports”
Direct Severe Guidance from SSEFProbability of Severe Thunderstorms based on “synthetic reports”
Direct Severe Guidance from SSEFProbability of Severe Thunderstorms based on “synthetic reports”
Summary: Ensemble Applications in High Impact Forecasting
• Ensemble approach to forecasting has many similarities to the deterministic approach– Ingredients based inputs– Diagnostic and parameter evaluation
• Ensembles contribute appropriate levels of confidence to the forecast process– Ability to view diagnostics and impacts in probability space
• Calibration of ensemble output can remove systematic biases and improve the spread
• Ensemble techniques scale to the problem of interest (weeks, days, or hours)