Access the full text.
Sign up today, get DeepDyve free for 14 days.
Daniel Miller (2000)
A Detailed Look at Extreme Wind Damage in Derecho Events
R. Schumacher, Richard Johnson (2005)
Organization and Environmental Properties of Extreme-Rain-Producing Mesoscale Convective SystemsMonthly Weather Review, 133
D. Atlas (1976)
severe local stormsBulletin of the American Meteorological Society, 57
I. Jirak, W. Cotton, Ray McAnelly (2003)
Satellite and Radar Survey of Mesoscale Convective System DevelopmentMonthly Weather Review, 131
James Duke, Joseph Rogash (1992)
Multiscale Review of the Development and Early Evolution of the 9 April 1991 DerechoWeather and Forecasting, 7
B. Storm, M. Parker, D. Jorgensen (2007)
A Convective Line with Leading Stratiform Precipitation from BAMEXMonthly Weather Review, 135
(2005)
2005b: Tornadoes from squall lines and bow echoes
B. Smull, R. Houze (1987)
Rear Inflow in Squall Lines with Trailing Stratiform PrecipitationMonthly Weather Review, 115
R. Johns, C. Doswell (1992)
Severe Local Storms ForecastingWeather and Forecasting, 7
R. Trapp, G. Stumpf, K. Manross (2005)
A Reassessment of the Percentage of Tornadic MesocyclonesWeather and Forecasting, 20
Glickman (2000)
Glossary of Meteorology.
R. Trapp, Dustan Wheatley, Nolan Atkins, R. Przybylinski, R. Wolf (2006)
Buyer Beware: Some Words of Caution on the Use of Severe Wind Reports in Postevent Assessment and ResearchWeather and Forecasting, 21
H. Bluestein, Michael Jain (1985)
Formation of Mesoscale Lines of Pirecipitation: Severe Squall Lines in Oklahoma during the SpringJournal of the Atmospheric Sciences, 42
M. Parker (2007)
Simulated Convective Lines with Parallel Stratiform Precipitation. Part I: An Archetype for Convection in Along-Line ShearJournal of the Atmospheric Sciences, 64
Brian Klimowski, Matthew Bunkers, M. Hjelmfelt, Josiah Covert (2003)
Severe Convective Windstorms over the Northern High Plains of the United StatesWeather and Forecasting, 18
G. Forbes (1981)
On the Reliability of Hook Echoes as Tornado IndicatorsMonthly Weather Review, 109
M. Baldwin, J. Kain, S. Lakshmivarahan (2005)
Development of an Automated Classification Procedure for Rainfall SystemsMonthly Weather Review, 133
P. Markowski (2002)
Hook Echoes and Rear-Flank Downdrafts: A ReviewMonthly Weather Review, 130
M. Parker, Richard Johnson (2000)
Organizational Modes of Midlatitude Mesoscale Convective SystemsMonthly Weather Review, 128
A. Moller, C. Doswell, Michael Foster, Gary Woodall (1994)
The Operational Recognition of Supercell Thunderstorm Environments and Storm StructuresWeather and Forecasting, 9
R. Trapp, Sarah Tessendorf, Elaine Godfrey, H. Brooks (2005)
Tornadoes from squall lines and bow echoes. Part I: Climatological distributionWeather and Forecasting, 20
G. Stumpf, A. Witt, E. Mitchell, P. Spencer, James Johnson, M. Eilts, K. Thomas, D. Burgess (1998)
The National Severe Storms Laboratory Mesocyclone Detection Algorithm for the WSR-88D*Weather and Forecasting, 13
C. Finley (2008)
Mobile mesonet observations of an intense RFD and multiple RFD gust fronts in the May 23 Quinter, Kansas tornadic supercell during TWISTEX 2008
Stephanie Verbout, H. Brooks, L. Leslie, D. Schultz (2006)
Evolution of the U.S. Tornado Database: 1954–2003Weather and Forecasting, 21
D. Burgess, L. Lemon (1990)
Severe thunderstorm detection by radar
Weiss (2002)
An examination of severe thunderstorm wind report climatology: 1970–1999.
W. Gallus, Nathan Snook, Elise Johnson (2008)
Spring and Summer Severe Weather Reports over the Midwest as a Function of Convective Mode: A Preliminary StudyWeather and Forecasting, 23
E. Mitchell, S. Vasiloff, G. Stumpf, A. Witt, M. Eilts, J. Johnson, K. Thomas (1998)
The National Severe Storms Laboratory Tornado Detection AlgorithmWeather and Forecasting, 13
(2002)
An examination of severe thunderstorm wind report climatology
J. Grams, W. Gallus, S. Koch, Linda Wharton, Andrew Loughe, E. Ebert (2006)
The use of a modified Ebert-McBride technique to evaluate mesoscale model QPF as a function of convective system morphology during IHOP 2002Weather and Forecasting, 21
C. Doswell, D. Burgess (1988)
On Some Issues of United States Tornado ClimatologyMonthly Weather Review, 116
Doswell (1993)
Tornadoes and tornadic storms: A review of conceptual models.
This study compares severe weather reports associated with the nine convective system morphologies used in a recent study by Gallus et al. to an additional morphology, supercell storms. As in that previous study, all convective systems occurring in a 10-state region covering parts of the Midwestern United States and central plains were classified according to their dominant morphology, and severe weather reports associated with each morphology were then analyzed. Unlike the previous study, which examined systems from 2002, the time period over which the climatology was performed was shifted to 2007 to allow access to radar algorithm information needed to classify a storm as a supercell. Archived radar imagery was used to classify systems as nonlinear convective events, isolated cells, clusters of cells, broken lines of cells, squall lines with no stratiform precipitation, trailing stratiform precipitation, parallel stratiform precipitation, and leading stratiform precipitation, and bow echoes. In addition, the three cellular classifications were subdivided to allow an analysis of severe weather reports for events in which supercells were present and those in which they were not. As in the earlier study, all morphologies were found to pose some risk of severe weather, and differences in the two datasets were generally small. The 2007 climatology confirmed the theory that supercellular systems produce severe weather more frequently than other morphologies, and also produce more intense severe weather. Supercell systems were especially prolific producers of tornadoes and hail relative to all other morphologies, but also produced severe wind and flooding much more often than nonsupercell cellular morphologies. These results suggest that it is important to differentiate between cellular morphologies containing rotation and those that do not when associating severe weather reports with convective morphology.
Weather and Forecasting – American Meteorological Society
Published: Jul 23, 2009
Read and print from thousands of top scholarly journals.
Already have an account? Log in
Bookmark this article. You can see your Bookmarks on your DeepDyve Library.
To save an article, log in first, or sign up for a DeepDyve account if you don’t already have one.
Copy and paste the desired citation format or use the link below to download a file formatted for EndNote
Access the full text.
Sign up today, get DeepDyve free for 14 days.
All DeepDyve websites use cookies to improve your online experience. They were placed on your computer when you launched this website. You can change your cookie settings through your browser.