Search Results
. J. Kocin, 1983: An interactive Barnes objective map analysis scheme for use with satellite and conventional data. J. Climate Appl. Meteor., 22, 1487 1503.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.Mahoney, E. A., and R. Schaar, 1993: WSR-88D scan strategy impacts on the vertically integrated liquid product. Preprints, 26th Int. Conf on Radar Meteorology, Norman, OK
. J. Kocin, 1983: An interactive Barnes objective map analysis scheme for use with satellite and conventional data. J. Climate Appl. Meteor., 22, 1487 1503.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.Mahoney, E. A., and R. Schaar, 1993: WSR-88D scan strategy impacts on the vertically integrated liquid product. Preprints, 26th Int. Conf on Radar Meteorology, Norman, OK
. Remote Sens. , 30 , 2 – 27 . 10.1109/36.124212 Kuo, Y-H. , Reed R. J. , and Low-Nam S. , 1992 : Thermal structure and airflow in a model simulation of an occluded marine cyclone. Mon. Wea. Rev. , 120 , 2280 – 2297 . 10.1175/1520-0493(1992)120<2280:TSAAIA>2.0.CO;2 Lee, D. L. , and Wilhelmson R. B. , 1997 : The numerical simulation of non-supercell tornadogenesis. Part I: Initiation and evolution of pretornadic misocyclone circulations along a dry outflow boundary. J. Atmos. Sci
. Remote Sens. , 30 , 2 – 27 . 10.1109/36.124212 Kuo, Y-H. , Reed R. J. , and Low-Nam S. , 1992 : Thermal structure and airflow in a model simulation of an occluded marine cyclone. Mon. Wea. Rev. , 120 , 2280 – 2297 . 10.1175/1520-0493(1992)120<2280:TSAAIA>2.0.CO;2 Lee, D. L. , and Wilhelmson R. B. , 1997 : The numerical simulation of non-supercell tornadogenesis. Part I: Initiation and evolution of pretornadic misocyclone circulations along a dry outflow boundary. J. Atmos. Sci
); the collision of surface convergence boundaries is considered a significant factor in the rapid intensification of storms and for tornadogenesis (see Sills et al. 2004 and their references). The WDSS-based fields provide crucial information on the likelihood for specific types of severe weather to occur. At this time period, the likelihood values for tornadoes ( Fig. 12c ) and large hail ( Fig. 12e ) are very high, ranging from 0.6 to 1.0 and 1.0, respectively. And although the mesocyclonic
); the collision of surface convergence boundaries is considered a significant factor in the rapid intensification of storms and for tornadogenesis (see Sills et al. 2004 and their references). The WDSS-based fields provide crucial information on the likelihood for specific types of severe weather to occur. At this time period, the likelihood values for tornadoes ( Fig. 12c ) and large hail ( Fig. 12e ) are very high, ranging from 0.6 to 1.0 and 1.0, respectively. And although the mesocyclonic
. Climate Extremes , 20 , 81 – 91 , https://doi.org/10.1016/j.wace.2018.03.002 . 10.1016/j.wace.2018.03.002 Markowski , P. , and Y. Richardson , 2009 : Tornadogenesis: Our current understanding, forecasting considerations, and questions to guide future research . Atmos. Res. , 93 , 3 – 10 , https://doi.org/10.1016/j.atmosres.2008.09.015 . 10.1016/j.atmosres.2008.09.015 May , O. , and A. Bigham , 2012 : After the storm: Personal experiences following an EF4 tornado . J. Pediatr. Nurs
. Climate Extremes , 20 , 81 – 91 , https://doi.org/10.1016/j.wace.2018.03.002 . 10.1016/j.wace.2018.03.002 Markowski , P. , and Y. Richardson , 2009 : Tornadogenesis: Our current understanding, forecasting considerations, and questions to guide future research . Atmos. Res. , 93 , 3 – 10 , https://doi.org/10.1016/j.atmosres.2008.09.015 . 10.1016/j.atmosres.2008.09.015 May , O. , and A. Bigham , 2012 : After the storm: Personal experiences following an EF4 tornado . J. Pediatr. Nurs
.Brandes, E. A., 1978: Mesocyclone evolution and tornadogenesis:Some observations. Mon. Wea. Rev., 106, 995-1011.Browning, K. A., 1980: Review of local weather forecasting. Proc. Roy. Soc. London, A371, 197-211.--., 1982: Nowcasting. Academic Press, 256 pp.Byers, H. R., and R. R. Braham, Jr., 1949: The Thunderstorm. U.S. Govt. Printing Office, Washington, DC, 287 pp.Chahine, M. T., 1968: Determination of the temperature profile in an atmosphere from its outgoing radiance. J. Opt. Soc.' Amer., 58
.Brandes, E. A., 1978: Mesocyclone evolution and tornadogenesis:Some observations. Mon. Wea. Rev., 106, 995-1011.Browning, K. A., 1980: Review of local weather forecasting. Proc. Roy. Soc. London, A371, 197-211.--., 1982: Nowcasting. Academic Press, 256 pp.Byers, H. R., and R. R. Braham, Jr., 1949: The Thunderstorm. U.S. Govt. Printing Office, Washington, DC, 287 pp.Chahine, M. T., 1968: Determination of the temperature profile in an atmosphere from its outgoing radiance. J. Opt. Soc.' Amer., 58
Doswell C. A. III , 1979 : Severe thunderstorm evolution and mesocyclone structure as related to tornadogenesis . Mon. Wea. Rev. , 107 , 1184 – 1197 , doi: 10.1175/1520-0493(1979)107<1184:STEAMS>2.0.CO;2 . Lilly, D. K. , 1986 : The structure, energetics and propagation of rotating convective storms. Part II: Helicity and storm stabilization . J. Atmos. Sci. , 43 , 126 – 140 , doi: 10.1175/1520-0469(1986)043<0126:TSEAPO>2.0.CO;2 . Maddox, R. A. , Hoxit L. R. , and Chappell C. F
Doswell C. A. III , 1979 : Severe thunderstorm evolution and mesocyclone structure as related to tornadogenesis . Mon. Wea. Rev. , 107 , 1184 – 1197 , doi: 10.1175/1520-0493(1979)107<1184:STEAMS>2.0.CO;2 . Lilly, D. K. , 1986 : The structure, energetics and propagation of rotating convective storms. Part II: Helicity and storm stabilization . J. Atmos. Sci. , 43 , 126 – 140 , doi: 10.1175/1520-0469(1986)043<0126:TSEAPO>2.0.CO;2 . Maddox, R. A. , Hoxit L. R. , and Chappell C. F
was due to their warning criteria not being fully satisfied. For example, in case 1, P 3 said that she was “flirting with the criteria” since the storm appeared “more marginal,” and P 4 went ahead with issuing a tornado warning in case 2 despite being “not sure [that the] environment was conducive” for tornadogenesis. Similarly, some experimental participants found themselves making warning decisions without confidence. During case 2, P 10 questioned the severe potential of a storm on which
was due to their warning criteria not being fully satisfied. For example, in case 1, P 3 said that she was “flirting with the criteria” since the storm appeared “more marginal,” and P 4 went ahead with issuing a tornado warning in case 2 despite being “not sure [that the] environment was conducive” for tornadogenesis. Similarly, some experimental participants found themselves making warning decisions without confidence. During case 2, P 10 questioned the severe potential of a storm on which
numerically simulated idealized squall line to the vertical distribution of aerosols . J. Atmos. Sci. , 71 , 4581 – 4596 , doi: 10.1175/JAS-D-14-0068.1 . Lebo, Z. J. , and Morrison H. , 2014 : Dynamical effects of aerosol perturbations on simulated idealized squall lines . Mon. Wea. Rev. , 142 , 991 – 1009 , doi: 10.1175/MWR-D-13-00156.1 . Lee, B. D. , and Wilhelmson R. B. , 1997 : The numerical simulation of non-supercell tornadogenesis. Part I: Initiation and evolution of pretornadic
numerically simulated idealized squall line to the vertical distribution of aerosols . J. Atmos. Sci. , 71 , 4581 – 4596 , doi: 10.1175/JAS-D-14-0068.1 . Lebo, Z. J. , and Morrison H. , 2014 : Dynamical effects of aerosol perturbations on simulated idealized squall lines . Mon. Wea. Rev. , 142 , 991 – 1009 , doi: 10.1175/MWR-D-13-00156.1 . Lee, B. D. , and Wilhelmson R. B. , 1997 : The numerical simulation of non-supercell tornadogenesis. Part I: Initiation and evolution of pretornadic
: Severe thunderstorm evolution and mesocyclone structure as related to tornadogenesis . Mon. Wea. Rev. , 107 , 1184 – 1197 , doi: 10.1175/1520-0493(1979)107<1184:STEAMS>2.0.CO;2 . Nelson, S. P. , and Young S. K. , 1979 : Characteristics of Oklahoma hailfalls and hailstorms . J. Appl. Meteor. , 18 , 339 – 347 , doi: 10.1175/1520-0450(1979)018<0339:COOHAH>2.0.CO;2 . Outinen, K. , and Teittinen J. , 2008 : Polarimetric radar observations of a tornadic supercell in Finland. Preprints
: Severe thunderstorm evolution and mesocyclone structure as related to tornadogenesis . Mon. Wea. Rev. , 107 , 1184 – 1197 , doi: 10.1175/1520-0493(1979)107<1184:STEAMS>2.0.CO;2 . Nelson, S. P. , and Young S. K. , 1979 : Characteristics of Oklahoma hailfalls and hailstorms . J. Appl. Meteor. , 18 , 339 – 347 , doi: 10.1175/1520-0450(1979)018<0339:COOHAH>2.0.CO;2 . Outinen, K. , and Teittinen J. , 2008 : Polarimetric radar observations of a tornadic supercell in Finland. Preprints
Representation of Cumulus Convection in Numerical Models . Meteor. Monogr., No. 46, Amer. Meteor. Soc., 246 pp . 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. , 58 , 1597 – 1629 . 10.1175/1520-0469(2001)058<1597:NSOTIA>2.0.CO;2 Fritsch, J. M. , and Coauthors . 1998 : Quantitative precipitation forecasting: Report of the Eighth
Representation of Cumulus Convection in Numerical Models . Meteor. Monogr., No. 46, Amer. Meteor. Soc., 246 pp . 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. , 58 , 1597 – 1629 . 10.1175/1520-0469(2001)058<1597:NSOTIA>2.0.CO;2 Fritsch, J. M. , and Coauthors . 1998 : Quantitative precipitation forecasting: Report of the Eighth
