Storm Surge Modeling and Forecasting

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Presentation transcript:

Storm Surge Modeling and Forecasting LTJG Jeffrey Pereira, NOAA Storm Surge Unit National Hurricane Center NOAA Storm Surge Workshop May 2011

Modeling Surge Statistical Deterministic Numerical Models Utilize historical data to develop statistical relationships between surge and driving factors Necessary data is non-existent Deterministic Numerical Models Forecast surge based on solving physical equations Strongly dependent on accurate meteorological input Current uncertainty in tropical cyclone forecasts render such methods inaccurate Numerical Model Ensemble Many different runs of the same model but with different conditions (family of storms) Best approach for determining storm surge vulnerability for an area since it takes into account forecast uncertainty

SLOSH Sea, Lake, and Overland Surges from Hurricanes A computerized numerical model developed by the National Weather Service (NWS) to estimate storm surge heights (and winds) resulting from historical, hypothetical, or predicted hurricanes

SLOSH SLOSH does include: Flow through barriers/gaps/passes Deep passes between bodies of water Inland inundation (wet/dry cell) Overtopping of barrier systems, levees, and roads Coastal reflection (coastally trapped Kelvin waves) SLOSH does not include: Breaking waves/wave run-up Astronomical tide Operational runs can be run at different tide levels via an initial water level (anomaly) Normal river flow and rain

ADCIRC & SLOSH Overall flooding pattern very similar

Forecasting Surge All storm surge models are STRONGLY dependent on the accuracy of the meteorological input!!! Meteorological uncertainty will dominate over storm surge model specifications (physics, resolution, etc.) Different vertical datums/reference levels Storm surge is only one component in the real water level rise. Total water rise = surge + tides + waves + freshwater flow

Forecast Uncertainty

Hurricane Advisory – Approximately 12 hr. before landfall NHC TRACK ERROR 12 hr. OUT 133 mph, 933 mb. Hurricane Advisory – Approximately 12 hr. before landfall

Surge Based on NHC -12 hr. Advisory Rmax=25 mi (forecast) Surge Based on NHC -12 hr. Advisory

Actual Hurricane Track 30 mi. E of -12 hr. Advisory Forecast Track ACTUAL TRACK TRACK FORECAST 133 mph, 933 mb. Actual Hurricane Track 30 mi. E of -12 hr. Advisory Forecast Track

Surge Based on NHC Storm Best Track Rmax=40 mi Surge Based on NHC Storm Best Track

RMW = 25 mi., “Average” Size

RMW = 6 mi.

Alternative to Single Runs Atlas of pre-computed surge maps based on: Different directions of motion Different landfall locations Different intensities Different storm sizes Different forward speeds

Ensemble Products 1. MEOWs Maximum Envelopes Of Water 2. MOMs Maximum Of the MEOWs 3. P-surge Probabilistic Storm Surge

Maximum Envelope Of Water MEOW Maximum Envelope Of Water

Maximum Envelope Of Water User selects: Category (Cat 3) Landfall direction (wnw) Forward speed (15 mph) Initial tide (High)

Maximum Envelope Of Water User selects: Category (Cat 3) Landfall direction (wnw) Forward speed (15 mph) Initial tide (High)

Maximum Envelope Of Water User selects: Category (Cat 3) Landfall direction (wnw) Forward speed (15 mph) Initial tide (High)

MOM Maximum Of the MEOWs

MOM User selects: Category (Cat 3)

Probabilistic Storm Surge Use an ensemble of SLOSH runs to create probabilistic storm surge (p-surge) Intended to be used operationally so it is based on NHC’s official advisory P-surge’s ensemble perturbations are determined by statistics of past performance of the advisories

Error Incorporated in P-Surge Ensemble based on distributions of: Cross track error (impacts Location) Along track error (impacts Forward Speed, Timing) Intensity error (impacts Pressure) Rmax error (impacts Size)

Cross-Track Error

Other Parameters Size: Small (30%), Medium (40%), Large (30%) Forward Speed: Fast (30%), Medium (40%), Slow (30%) Intensity: Strong (30%), Medium (40%), Weak (30%)

When is it Available? Whenever a hurricane watch or warning is in effect Available about 30 minutes after the advisory release time

Understanding/Using Probability The number one argument against using probability is that users do not understand how to interpret low probabilities of an extreme event Would you offer to pick up free lunch if there is a 20% chance of you being involved in a fatal car accident along the way? 27

Surge Based on NHC -12 hr. Advisory Deterministic SLOSH run shows limited surge threat to Pensacola area Rmax=25 mi (forecast) Surge Based on NHC -12 hr. Advisory

Probabilistic product shows considerable surge threat to Pensacola area

Actual storm caused highest surge in Pensacola area

NHC Advisory/ NWS Local Statements Surge Guidance Timeframe NHC Storm Surge Product Decision Support Wedge NHC Advisory/ NWS Local Statements Probabilistic Storm Surge *MEOWs *MOMs Tier 1 Response < 48 h of landfall Tier 3 Planning/Mitigation > 120 h of landfall Tier 2 Readiness 48 h – 120 h of landfall