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Administration through the Hollings Scholarship Program

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Presentation on theme: "Administration through the Hollings Scholarship Program"— Presentation transcript:

1 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

2 Outline Project Purpose Background Methodology Results Next Steps
Conclusion Acknowledgements

3 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.

4 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

5 What I have done: Examined environments of non-significant tornado events. Made comparison to significant tornado environments.

6 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…

7 As pictorially defined here:

8 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.

9 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.

10 Some days were very small events
Tornado Tracks + Damaging Winds Severe Hail

11 Others were widespread outbreaks
Tornado Tracks + Damaging Winds Severe Hail

12 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

13 Data Collection Archived: Nearest: Favored Warm Sector Surface Plots
Radiosonde Data Nearest: Spatially With Time Favored Warm Sector

14 Data Organized in Excel

15 Many Graphs Were Created

16 Thousands of Gempak Maps

17 Box and Whiskers Format
90th percentile Middle 50% 10th percentile

18 Results Temps, dewpoints, thickness, and theta-e all very similar at all levels for all 4 cases!

19 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

20 Wind Speed – Best Differentiator

21 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.

22 Wind Direction Poor differentiator All veered with height

23 Wind Direction Unexpected finding:
Significant tornado events had less veering than the others from 700mb to 500mb.

24 Next Steps Comparison can be made for instability, helicity and other convective parameters. Thereafter, a final paper will be published.

25 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.

26 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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