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Administration through the Hollings Scholarship Program
“Environments of Non-Significant Cool Season Severe Weather Events in the Southeastern United States” William A. Komaromi University at Albany Storm Prediction Center David Imy & Jared Guyer This research was supported by an appointment to the National Oceanic & Atmospheric Administration through the Hollings Scholarship Program 9/21/2018
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Outline Project Purpose Background Methodology Results Next Steps
Conclusion Acknowledgements
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Project Purpose To help Storm Prediction Center forecasters better differentiate the subtle differences between significant tornado and non-significant tornado environments during the Southeastern United States cool season.
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Background 2005 Kar’retta Venable of Jackson State University at Jackson, Mississippi 2006 Amanda Kis of University of Wisconsin at Madison F2 or stronger tornadoes Environmental parameters
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What I have done: Examined environments of non-significant tornado events. Made comparison to significant tornado environments.
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Cases were identified that occurred:
Methodology Cases were identified that occurred: During a 12z to 12z timeframe In the cool season months from October 1st to the end of February Geographically within a Southeast U.S. domain…
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As pictorially defined here:
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Anticipated Outcome Subtle differences
Significant tornado days will have… Higher wind speeds More directional shear Warmer and moister low-levels Colder temperatures aloft … than non-significant tornado days.
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What cases did I look for?
Days with 2+ tornadoes or 15+ severe hail and/or wind, but with no tornadoes of F2 or stronger intensity.
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Some days were very small events
Tornado Tracks + Damaging Winds Severe Hail
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Others were widespread outbreaks
Tornado Tracks + Damaging Winds Severe Hail
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Event days were broken up into five categories:
Significant Tornado Days (F2+): 150 cases Non-significant tornado days: 145 cases Weak Tornado Days (F0, F1): 103 cases Severe Hail / Wind Only Days: 42 cases All tropical events were removed
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Data Collection Archived: Nearest: Favored Warm Sector Surface Plots
Radiosonde Data Nearest: Spatially With Time Favored Warm Sector
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Data Organized in Excel
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Many Graphs Were Created
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Thousands of Gempak Maps
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Box and Whiskers Format
90th percentile Middle 50% 10th percentile
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Results Temps, dewpoints, thickness, and theta-e all very similar at all levels for all 4 cases!
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Results: Significant tornado and non-significant tornado events:
Surface Temps 65–75°F Surface Dewpoints 60–70°F mb Thickness 5600–5700m 925mb Theta-e K 700mb Temps 1-7°C
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Wind Speed – Best Differentiator
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Wind Speed – Best Indicator
Wind speeds of: 40+ kts at 850mb 45+ kts at 700mb 60+ kts at 500mb Represent middle 50% of significant tornado events, but near the outer 90th percentile in non-significant tornado events.
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Wind Direction Poor differentiator All veered with height
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Wind Direction Unexpected finding:
Significant tornado events had less veering than the others from 700mb to 500mb.
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Next Steps Comparison can be made for instability, helicity and other convective parameters. Thereafter, a final paper will be published.
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Conclusions The greatest differentiator between significant and non-significant tornado events was stronger winds at 850, 700 and 500 mb. Overall differences in all other parameters are very subtle.
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Acknowledgements Galway, J. G., and A. Pearson, 1981: Winter tornado outbreaks. Mon. Wea. Rev., 109, Guyer, Jared L., Imy, David A., Kis, Amanda, and Venable, Kar’retta, 2006: Cool Season Significant (F2-F5) Tornadoes in the Gulf Coast States. Johns, R. H., and C. A. Doswell III, 1992: Severe local storms forecasting. Wea. And Forecasting, 7, National Climatic Data Center, Plymouth State University Meteorology Program, North American Regional Reanalysis Homepage, Vescio, M. D., and R. L. Thompson, 1993: Some meteorological conditions associated with isolated F3-F5 tornadoes in the cool season. Preprints, 19th Conf. On Severe Local Storms, Minneapolis, MN, 2-4.
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