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Lightning Forecasting at the Storm Prediction Center. Joe Schaefer with help from Phillip Bothwell, David Bright and Russell Schneider. Current uses of the NLDN by the SPC. First strike detection – convective initiation Subjective measure of convective intensity & trend
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Lightning Forecasting at the Storm Prediction Center Joe Schaefer with help from Phillip Bothwell, David Bright and Russell Schneider
Current uses of the NLDN by the SPC • First strike detection – convective initiation • Subjective measure of convective intensity & trend • Verification and validation of thunderstorms • Detection of convection in regions of sparse radar coverage (esp. for Fire Weather)
SPC Lightning Forecasts • General Thunder in Convective Outlook • “Enhanced Thunder” • Presently experimental on Internet • Operational Product next year • Fire Weather Outlook Two types of Internal Thunderstorm Guidance
Enhanced Thunder 19 July 2005 200000Z – 201200Z
Ensemble Forecasts • Current SPC SREF processing • All operational computations on NOAA CCS • SREF products specialized for the national mission of the SPC • 16 member SREF (1 time-lagged Eta member) • Include the -3 hr operational Eta in all calculations • Add the +3 hr operational Eta to spaghetti plots
CLOUD PHYSICS THUNDER PARAMETER Percent of members with appreciable CAPE in the 0oC to -20oC layer SREF MEAN CPTP = 1 (DASHED) SREF PROB CPTP >= 1 (SOLID & FILLED) F15 SREF PROBABILITY CLOUD PHYSICS THUNDER PARAMETER >= 1
- Pr (CPTP) >= 1 x Pr (PCPN) >= .01” Uncalibrated probability of lightning F15 SREF 3-hr COMBINED PROBABILITY OF LIGHTNING
F15 SREF 3-hr COMBINED PROBABILITY OF LIGHTNING (Calibrated) & LIGHTNING STRIKES
Statistical Forecasts Based on Phillip Bothwell’s Dissertation work • Perfect Prog Forecast Technique Principal Component Analysis determines predictors Logistic regression • 40 km grid resolution at 3 hour time intervals • Uses Lightning Climatology (no knowledge of ongoing activity Forecasts • Probability of 1 or more CG flashes • Probability of 100 or more CG flashes.
OBJECTIVES • Technique applicable to ANYanalysis or gridded data set (i.e., forecast for the next 3 hours… 57 to 60 hours, or any time period in between) • System can run on data fromANY forecast model. inter-model comparisons (different models…e.g., RUC and ETA) intra-model comparisons (different cycles of same model). • Distinguish low lightning producers from high producers
12-15UTC 15-18UTC LTG CLIMATOLOGY: Probability of one or more CG flashes / 40x40 km grid box / 3 hrs. Centered on July 22 Relative minimum during daytime hours Relative maximum during daytime hours 18-21 UTC 21-00UTC
00-03UTC 03-06UTC LTG CLIMATOLOGY: Probability of one or more CG flashes / 40x40 km grid box / 3 hrs. Centered on July 22 Relative maximum during overnight hours Relative minimum during overnight hours 06-09UTC 09-12UTC
57-60 Hour Lightning Forecast 12Z July 13, 2004 Forecast Observed
There can be a big difference between storms that produce only one flash and…
… those that have large numbers of flashes! Previous attempts at predicting events with significant flash rates have not met with much success! NOAA Photo Library NWS Historical Collection
Significant CG Lightning Events100 or more CG flashes/40x40 km/3 hrs • Kempf and Krider (2003) as well as others have found a strong connection between daily rain volumes and corresponding counts of CG lightning • Intense areas of CG lightning can often be associated with strong to severe storms
Probability of 100 or more CG Flashes 9-12 hour Forecast 18Z Sep. 18, 2004 Climatology 03 Z – 06Z 5 Days Centered on Sep. 20 Solid Probability 21,%, 2%, 5% Dashed Observed 100,200,399 Flashes
Future use of Lightning Data • Become more quantitative • Track development & evolution of total lightning within individual thunderstorms • Prediction of critical lightning characteristics • Positive CG Strokes – Fire Weather (house fires?) • Forecasts of severe lightning events • We need to learn more …