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Dereka Carroll-Smith
,
Robert J. Trapp
, and
James M. Done

.1175/BAMS-D-12-00074.1 . 10.1175/BAMS-D-12-00074.1 Rhodes , C. L. , and J. C. Senkbeil , 2014 : Factors contributing to tornadogenesis in landfalling Gulf of Mexico tropical cyclones . Meteor. Appl. , 21 , 940 – 947 , https://doi.org/10.1002/met.1437 . 10.1002/met.1437 Sato , T. , F. Kimura , and A. Kitoh , 2007 : Projection of global warming onto regional precipitation over Mongolia using a regional climate model . J. Hydrol. , 333 , 144 – 154 , https://doi.org/10.1016/j

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Toshinori Aoyagi
and
Naoko Seino

urban surface exchange parameterisation for mesoscale models . Bound.-Layer Meteor. , 104 , 261 – 304 . Mashiko , W. , H. Niino , and T. Kato , 2009 : Numerical simulation of tornadogenesis in an outer-rainband minisupercell of Typhoon Shanshan on 17 September 2006 . Mon. Wea. Rev. , 137 , 4238 – 4260 . Masson , V. , 2000 : A physically-based scheme for the urban energy budget in atmospheric models . Bound.-Layer Meteor. , 94 , 357 – 397 . Masson , V. , C. S. B. Grimmond

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Matthew R. Kumjian
,
Yvette P. Richardson
,
Traeger Meyer
,
Karen A. Kosiba
, and
Joshua Wurman

.1175/1520-0477(1992)073<1365:OPTDPR>2.0.CO;2 Hogan , R. J. , N. Gaussian , and A. J. Illingworth , 2005 : Stratocumulus liquid water content from dual-wavelength radar . J. Atmos. Oceanic Technol. , 22 , 1207 – 1218 , https://doi.org/10.1175/JTECH1768.1 . 10.1175/JTECH1768.1 Houser , J. , H. B. Bluestein , and J. C. Snyder , 2015 : Rapid-scan, polarimetric, Doppler radar observations of tornadogenesis and tornado dissipation in a tornado supercell: The “El Reno, Oklahoma” storm of 24 May 2011 . Mon. Wea

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Jeffrey C. Snyder
,
Howard B. Bluestein
,
Daniel T. Dawson II
, and
Youngsun Jung

.1175/1520-0493(2003)131<2394:RRFTSO>2.0.CO;2 Burgess , D. W. , E. R. Mansell , C. M. Schwarz , and B. J. Allen , 2010 : Tornado and tornadogenesis events seen by the NOXP X-band, dual-polarization radar during VORTEX2 2010. 25th Conf. on Severe Local Storms , Denver, CO, Amer. Meteor. Soc., 5.2. [Available online at https://ams.confex.com/ams/25SLS/techprogram/paper_176164.htm .] Carte , A. E. , and R. E. Kidder , 1966 : Transvaal hailstones . Quart. J. Roy. Meteor. Soc. , 92 , 382 – 391 , doi: 10.1002/qj

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John Y. N. Cho
and
James M. Kurdzo

-00076.1 Kurdzo , J. M. , and Coauthors , 2017 : Observations of severe local storms and tornadoes with the atmospheric imaging radar . Bull. Amer. Meteor. Soc. , 98 , 915 – 935 , https://doi.org/10.1175/BAMS-D-15-00266.1 . 10.1175/BAMS-D-15-00266.1 Lemon , L. R. , and C. A. Doswell III , 1979 : Severe thunderstorm evolution and mesocyclone structure as related to tornadogenesis . Mon. Wea. Rev. , 107 , 1184 – 1197 , https://doi.org/10.1175/1520-0493(1979)107<1184:STEAMS>2.0.CO;2 . 10

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Matthew R. Kumjian
and
Alexander V. Ryzhkov

United States. Wea. Forecasting , 17 , 927 – 934 . Markowski , P. M. , J. Straka , and E. Rasmussen , 2002 : Direct surface thermodynamic observations within the rear-flank downdrafts of nontornadic and tornadic supercells. Mon. Wea. Rev. , 130 , 1692 – 1721 . Markowski , P. M. , J. M. Straka , and E. N. Rasmussen , 2003 : Tornadogenesis resulting from the transport of circulation by a downdraft: Idealized numerical simulations. J. Atmos. Sci. , 60 , 795 – 823

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Corey K. Potvin
,
Chris Broyles
,
Patrick S. Skinner
, and
Harold E. Brooks

models . J. Roy. Stat. Soc. , 75A , 139 – 159 , https://doi.org/10.1111/j.1467-9868.2012.01041.x . Hussain , M. , and I. Mamhud , 2019 : pyMannKendall: A Python package for non parametric Mann Kendall family of trend tests . J. Open Source Software , 4 , 1556 , https://doi.org/10.21105/joss.01556 . Lee , B. D. , and R. B. Wilhelmson , 1997 : The numerical simulation of non-supercell tornadogenesis. Part I: Initiation and evolution of pretornadic misocyclone circulations

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Roger Edwards
,
Harold E. Brooks
, and
Hannah Cohn

cautionary statement about data integrity (see more in section 4 ). This also underscores the need for caution in using bulk indices in terms of keenly understanding their components’ influences for research purposes, as well as for forecasting ( Doswell and Schultz 2006 ). c. Other tornado characteristics Other variables in ONETOR include deaths, injuries and reported tornadogenesis time. We analyzed some aspects of these with respect to the F and EF eras, with largely indefinite results. Violent

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Samuel J. Childs
and
Russ S. Schumacher

Divide topographical feature, an area of locally higher elevation between Colorado Springs and Denver, and converges with northwesterly flow moving downslope from the foothills to the north and west of Denver. This convergence leads to a localized area of vorticity, commonly known as the Denver Cyclone ( Szoke et al. 1984 ). As low-level vorticity is a key ingredient for tornadogenesis, it is not surprising that the Denver Cyclone was observed on many severe weather days across the Front Range during

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