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/NCAR 40-Year Reanalysis Project . Bull. Amer. Meteor. Soc. , 77 , 437 – 471 , doi: 10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO;2 . Klemp , J. B. , 1987 : Dynamics of tornadic thunderstorms . Annu. Rev. Fluid Mech. , 19 , 369 – 402 , doi: 10.1146/annurev.fl.19.010187.002101 . 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 , doi: 10
/NCAR 40-Year Reanalysis Project . Bull. Amer. Meteor. Soc. , 77 , 437 – 471 , doi: 10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO;2 . Klemp , J. B. , 1987 : Dynamics of tornadic thunderstorms . Annu. Rev. Fluid Mech. , 19 , 369 – 402 , doi: 10.1146/annurev.fl.19.010187.002101 . 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 , doi: 10
.2 . Klemp , J. B. , and R. B. Wilhelmson , 1978 : Simulations of right- and left-moving storms produced through storm splitting. J. Atmos. Sci. , 35 , 1097 – 1110 . 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 . Lenning , E. , H. E. Fuelberg , and A. I. Watson , 1998 : An evaluation of WSR-88D severe hail algorithms along the northeastern Gulf Coast
.2 . Klemp , J. B. , and R. B. Wilhelmson , 1978 : Simulations of right- and left-moving storms produced through storm splitting. J. Atmos. Sci. , 35 , 1097 – 1110 . 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 . Lenning , E. , H. E. Fuelberg , and A. I. Watson , 1998 : An evaluation of WSR-88D severe hail algorithms along the northeastern Gulf Coast
important insight regarding the mechanisms that led to tornadogenesis. Weather radar analysis confirmed that the parent storm was a left-moving cell. Reflectivity values were not particularly high and the storm was rather low topped as compared to “classic” supercells documented in other parts of the world (e.g., Kumjian and Ryzhkov 2008 ). Interestingly, the study by Held et al. (2010) reports further examples of supercells with relatively low tops over SP during the cold seasons (austral autumn and
important insight regarding the mechanisms that led to tornadogenesis. Weather radar analysis confirmed that the parent storm was a left-moving cell. Reflectivity values were not particularly high and the storm was rather low topped as compared to “classic” supercells documented in other parts of the world (e.g., Kumjian and Ryzhkov 2008 ). Interestingly, the study by Held et al. (2010) reports further examples of supercells with relatively low tops over SP during the cold seasons (austral autumn and
