Overview
Warm air advection and convergence associated with low pressure over eastern Colorado led to severe thunderstorms that produced tornadoes in central Minnesota. Of the 15 tornadoes reported, an F2 was the strongest and caused the most damage in Buffalo Lake. Two inch hail was reported in Rock County and 1.75 inch hail was reported in Pope, Lyon, and Renville Counties. Also, the Minneapolis International Airport recorded wind gusts of 58 miles per hour. |
Tornadoes:
Lincoln, Yellow Medicine, Chippewa, Renville, Sibley, Meeker, Kandiyohi, and Pope Counties
Track Map
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In 2003, the Fujita (F) Scale was used to classify tornadoes into the following categories:
F0 Weak <73 mph |
F1 Moderate 73-112 mph |
F2 Significant 113-157 mph |
F3 Severe 158-206 mph |
F4 Extreme 207-260 mph |
F5 Catastrophic 261-318 mph |
Radar:
0.5, 1.5, and 2.4 degree tilts of storm relative motion and 0.5 degree reflectivity at 6:29 PM | 0.5 degree reflectivity and 1.5, 2.4, and 3.4 degree tilts of storm relative motion at 7:28 PM | Composite reflectivity (left) and 0.5 degree storm relative velocity (right) at 7:44 PM |
Storm Reports
Environment
A quasi-stationary frontal boundary extending from central Minnesota to northwest Kansas caused warm air advection and low-level convergence. Moist, buoyant air along with high values of low-level wind shear and CAPE, and low Lifted Condensation Levels (LCLs) created a favorable environment for severe storms and tornadoes.
National Weather Forecast Chart | Surface frontal boundary and METARs | LAPS LCLs |
LAPS 0-6 km wind shear | Surface CAPE showing high risk area | 7 PM 500 mb analysis |
7 PM 250 mb analysis |
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