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Comparison of Disdrometer and X-Band mobile radar observations in convective precipitation
Near-surface vortex structure in a tornado and in a sub-tornado-strength convective-storm vortex observed by a mobile, w-band radar during VORTEX2
Spatial extreme value analysis to project extremes of large-scale indicators for severe weather
An example of the use of mobile, Doppler radar data for tornado verification
High winds generated by bow echoes. Part II: The relationship between the mesovortices and damaging straight-line winds
Nebraska tornado, May 24, 2004 (DI02256) Photo by Bob Henson
Nebraska tornado, May 24, 2004 (DI02255) Photo by Bob Henson
Tornado Damage (DI01080)
Tornado Damage (DI01079)
Kinematic and microphysical evolution of the 29 June supercell during STEPS
Tornado (2 of 5) (DI00556), Photo by Linda Lusk
Tornado (1 of 5) (DI00555), Photo by Linda Lusk
Tornado (3 of 5) (DI00557), Photo by Linda Lusk
Tornado (4 of 5) (DI00558), Photo by Linda Lusk
Tornado (5 of 5) (DI00559), Photo by Linda Lusk
Texas tornado (DI00509), Photo by Harald Richter
Texas tornado (DI00512), Photo by Harald Richter
Texas tornado (DI00510), Photo by Harald Richter
Texas tornado (DI00514), Photo by Harald Richter
Texas tornado (DI00515), Photo by Harald Richter

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