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Tropical Cyclone Forecasts Dr. Richard J. Murnane Risk Prediction Initiative Bermuda Biological Station for Research, Inc.
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Hurricane Landfall in Miami and Dade County Cat 1&2Cat 3, 4, 5 19101930195019701990 Hurricane Landfall per Year 210210 Year Landsea, 1997
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Tropical Cyclone Seasonal Forecasting Strategy l Identify predictable global and local features that drive climate l Statistically relate features to tropical cyclone occurrence
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Outline l Background on tropical cyclones –Necessary conditions –Forecast parameters l Seasonal forecasts –Basin-wide –Landfall l Real-time hurricane intensity forecasts –Numerical prediction –Theoretical Maximum Potential Intensity
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Necessary Conditions l l Coriolis Effect l l Unstable Atmosphere l l Sea Surface Temperature > 26º C l l Trigger l l Little Vertical Wind Shear l l High Relative Humidity
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Major Climatic Features Affecting Atlantic Basin Hurricane Activity l El Ni l El Niño-Southern Oscillation (ENSO) l l Quasi-biennial Oscillation l l Sea Surface Temperature (SST) l l West Africa Rainfall l l Atmospheric Zonal Wind Anomalies l l Sea Level Atmospheric Pressure
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El Niño-Southern Oscillation Images from IRI web site Normal El Niño
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US Hurricane Landfalls Cat. 3 0.0 0.2 0.4 0.6 0.8 24680 Probability Number Landfalls Per Year El Niño Neutral El Viejo J. O’Brien & COAPS
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0.0 0.2 0.4 0.6 0.8 1.0 Cat 1Cat 2Cat 3 El Niño Neutral El Viejo Baroclinically Influenced Atlantic Storms: Hurricane Landfalls/year # Landfalls/year
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Tropical Only Atlantic Storms: Hurricane Landfalls/year # Landfalls/year 0.0 0.5 1.0 1.5 Cat 1Cat 2Cat 3 El Niño Neutral El Viejo
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Quasi-Biennial Oscillation (QBO) Arrows show stratospheric wind direction West Phase Enhanced Atlantic Hurricane Formation East Phase Suppressed Atlantic Hurricane Formation
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Sea Surface Temperature Climate Prediction Center
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Sea Surface Temperature Anomalies Climate Prediction Center
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Seasonal Atlantic Hurricane Activity (1886-1991) 0 100 200 May June July Aug Sept Oct Nov Dec Jan-Apr
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West African Rainfall Western Sahel Region Gulf of Guinea Region
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Sahel Rain (1899 – 1990) 19001920194019601980 Standard Deviation Landsea et al., 1992 Year 2 1 0 -2
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1949 – 1990 0.64 IHD 7 Driest Sahel Years7 Wettest Sahel Years 14.43 IHD Gray & Landsea, 1992 Intense Hurricanes vs. Sahel Rain
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Long-term Trends Year Standard Deviation N. Atlantic SST Anomaly NE Atlantic SLP Anomaly (neg) Sahel Rain Intense Hurricane Days 19501960197019801990 2 1 0 -2 Gray, 1998
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Basin-Wide Seasonal Forecasts
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Gray et al.’s Basin-wide Forecasts l Issued in: December, April, June, August l Forecast includes a variety of parameters: –Named Storms –Hurricanes, Hurricane Days –Intense Hurricanes, Intense Hurricane Days –Hurricane Destruction Potential –Net Tropical Cyclone Activity l Predictive Parameters Vary With Forecast
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Gray et al.’s ‘98 Atlantic Basin Forecasts
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Landsea, 1997
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Elsner’s Atlantic Basin Forecasts l Uses subset of Gray variables –Zonal winds –West African rainfall l Divides storms into tropical only and baroclinically influenced –assumes climatology for baroclinically influenced storms (per year) –assumes climatology for baroclinically influenced storms ( per year) –Predicts tropical only storms using OLS l Calculates intense hurricanes using Poisson regression
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Elsner et al. Forecast 1998 Atlantic Intense Hurricanes Elsner et al., 1998 01234560123456
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August ‘98 Forecasts
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Seasonal Landfall and Location Forecasts
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Gray Landfall Forecast l Divides coast into separate sections l Uses Atlantic Basin seasonal forecast of “Net Tropical Cyclone Activity” (NTC) and SST anomalies to calculate total landfall probability l Distributes total probability along coast based on landfall climatology
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Cat 1&2 Hurricane Landfalls Gray, 1998
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Intense Hurricane Landfalls Gray, 1998
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1998 Landfall % Probability Forecast 36 8 39 10.2 34 33 4 7 5 6 8 Gray, 1998
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Elsner Landfall Probability Forecasts l Uses “Logistic Regression” for predictions l Predictors include: –Zonal wind anomalies –Sea level pressures –QBO –West African rainfall
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1998 Location Forecast Elsner et al., 1998
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Hurricane Intensity Forecasts
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NHC Intensity Forecasts (1990-97) 25 20 15 10 5 Error (knots) 199019911992 1993 1994 199519961997 72 hours 48 hours 24 hours Avila, 1998 Year
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Ginis et al.’s Hurricane Forecasts l Based on Coupled Ocean-Atmosphere Model l Full Ocean Model Reproduces Air-Sea Interactions and Improves Intensity Forecasts
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Hurricane Opal Ginis, 1998
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Maximum Potential Intensity (MPI) l Developed by Emanuel and Bister l MPI Controlled by Environmental Factors, e.g.: –Sea Surface Temperature –Upper Atmosphere Temperature –Relative Humidity l Doesn’t account for forward motion
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Contours of Maximum Wind Speed (m/s) Emanuel and Bister, 1998 Sea Surface Temperature (ºC) Upper Atmosphere Temperature (ºC) 15 20 25 30 35 40 45 -100 -75 -50 -25
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Maximum Potential Winds (m/s) Emanuel and Bister, 1998
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Maximum Potential Wind (knots) Emanuel and Bister, 1998
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Conclusions l Many of the seasonal forecast parameters are related to the necessary conditions for tropical cyclone formation l Basin-wide seasonal forecasts are easier to make than landfall forecasts but they are of less relevance l Realistic representations of the ocean are needed to improve tropical cyclone intensity forecasts
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