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Walker S. Ashley
,
Alex M. Haberlie
, and
Jacob Strohm

have substantial societal impact ( Ashley et al. 2008 ), are difficult to forecast and warn ( Brotzge et al. 2013 ; Anderson-Frey et al. 2016 ), and often appear to occur in environments with ingredients not typically considered favorable for significant tornadogenesis ( Kis and Straka 2010 ). Though tornado counts with both QLCSs and non-QLCSs reach a minimum during the overnight, the proportion that are due to QLCSs rapidly increases from less than 15% during the afternoon/evening hours to over

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Andrew Moore

differing initial conditions) of the same atmospheric phenomenon can lead to insightful statistics. One such example is Coffer et al. (2017) , which examined tornadogenesis probabilities from a statistical perspective utilizing 30 unique CM1 simulations of tornadic and nontornadic supercells. To date, no studies have attempted to examine the statistical distribution of surface winds from WFTs using output from multiple high-resolution simulations in a manner similar to the Coffer et al. (2017) study

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Darrel M. Kingfield
and
Michael M. French

Programming Language . J. Open Res. Software , 4 , e25 , https://doi.org/10.5334/jors.119 . 10.5334/jors.119 Houser , J. L. , H. B. Bluestein , and J. C. Snyder , 2015 : Rapid-scan, polarimetric, Doppler radar observations of tornadogenesis and tornado dissipation in a tornadic supercell: The “El Reno, Oklahoma” storm of 24 May 2011 . Mon. Wea. Rev. , 143 , 2685 – 2710 , https://doi.org/10.1175/MWR-D-14-00253.1 . 10.1175/MWR-D-14-00253.1 Hubbert , J. C. , V. N. Bringi , L. D

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Scott A. Braun
and
John P. Monteverdi

related to tornadogenesis. Mort. Wea. Rev., 107, 1184-1197.Marwitz, J. D., 1972: The structure and motions of severe hailstorms: Part I. Supercell storms. J. Appl. Meteor., 11, 166-179.McGinley, J., 1986: Nowcasting mesoseale phenomena. Mesoscale Meteorology and Forecasting. Peter S. Ray, Ed., Amer. Meteor. Soc., 657-688.McNulty, R., 1978: On upper tropospheric kinematics and severe weather occurrence. Mon. Wea. Rev., 106, 662-672.Moncrieff, M. W., and J. S. A. Green, 1972: The propagation and

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Cameron J. Nixon
and
John T. Allen

, and J. F. Weaver , 1994 : Some noteworthy aspects of the Hesston, Kansas, tornado family of 13 March 1990 . Bull. Amer. Meteor. Soc. , 75 , 1007 – 1018 , https://doi.org/10.1175/1520-0477(1994)075<1007:SNAOTH>2.0.CO;2 . 10.1175/1520-0477(1994)075<1007:SNAOTH>2.0.CO;2 Dowell , D. C. , and H. B. Bluestein , 2002a : The 8 June 1995 McLean, Texas, storm. Part I: Observations of cyclic tornadogenesis . Mon. Wea. Rev. , 130 , 2626 – 2648 , https://doi.org/10

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Bartlett C. Hagemeyer

ridges to their northeast creating an asymmetrical wind pattern. Low-level winds increased significantly east of the lows, and a favorable shear environment for tornadogenesis developed well east of the lows in the overrunning zone. In each case the orientation and slow movement of the hybrid cyclones caused peninsular Florida to be in a favorable shear and moisture environment for tornado and excessive rain production for 12–18 h. Most of the tornadoes occurred in the overrunning zone very near or

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Mark D. Powell
and
Samuel H. Houston

.] WAMDI Group, 1988: The WAM model- A third-generation ocean wave prediction model. J. Phys. Oceanogr., 18, 1775- 1810. Willoughby, H. E., and P. G. Black, 1996: Hurricane Andrew in Florida: Dynamics of a disaster. Bull. Amer. Meteor. Soc., 77, 543- 549. , J. M. Masters, and C. W. Landsea, 1989: A record sea level pressure observed in Hurricane Gilbert. Mon. Wea. Rev., 117, 2824- 2828. Wilson, J. W., 1986: Tornadogenesis by nonprecipitation induced wind shear lines. Mon. Wea. Rev

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Adam J. French
and
Matthew D. Parker

. Wea. Forecasting , 16 , 329 – 342 . 10.1175/1520-0434(2001)016<0329:EODEUP>2.0.CO;2 Finley, C. A. , Cotton W. R. , and Pielke R. A. , 2001 : Numerical simulation of tornadogenesis in a high-precipitation supercell. Part I: Storm evolution and transition into a bow echo. J. Atmos. Sci. , 58 , 1597 – 1629 . 10.1175/1520-0469(2001)058<1597:NSOTIA>2.0.CO;2 Fujita, T. T. , 1978 : Manual of downburst identification for project NIMROD. SMRP Research Paper 117, University of Chicago, 104

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Brian A. Klimowski
,
Matthew J. Bunkers
,
Mark R. Hjelmfelt
, and
Josiah N. Covert

.1175/1520-0434(2001)016<0329:EODEUP>2.0.CO;2 Finley, C. A. , Cotton W. R. , and Pielke R. A. Sr. , 2001 : Numerical simulation of tornadogenesis in a high-precipitation supercell. Part I: Storm evolution and transition into a bow echo. J. Atmos. Sci. , 38 , 1597 – 1629 . Fujita, T. T. , 1978 : Manual of downburst identification for Project Nimrod. Satellite and Mesometeorology Research Paper 156, Dept. of Geophysical Sciences, University of Chicago, 104 pp . Fujita, T. T. , 1981 : Tornadoes and downbursts in

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Bruno Z. Ribeiro
,
Luiz A. T. Machado
,
Joao H. Huamán Ch.
,
Thiago S. Biscaro
,
Edmilson D. Freitas
,
Kathryn W. Mozer
, and
Steven J. Goodman

.1029/93JD01617 . 10.1029/93JD01617 Gatlin , P. N. , and S. J. Goodman , 2010 : A total lightning trending algorithm to identify severe thunderstorms . J. Atmos. Oceanic Technol. , 27 , 3 – 22 , https://doi.org/10.1175/2009JTECHA1286.1 . 10.1175/2009JTECHA1286.1 Goodman , S. J. , and K. R. Knupp , 1993 : Tornadogenesis via squall line and supercell interaction: The November 15, 1989 Huntsville, Alabama tornado. The Tornado: Its Structure, Dynamics, Prediction, and Hazards, Geophys. Monogr

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