Abstract
Features of the storm recorded and analyzed include the following: the movement and dissipation of a cloud band associated with an apparent rear-flank downdraft; a transition from a rather large funnel through an apparent dissipation to the formation of a narrow funnel, during which the damage on the ground was continuous; a period of interaction between the first and second tornadoes. -from Authors
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CITATION STYLE
Davies, J. M., Doswell, C. A., Burgess, D. W., & Weaver, J. F. (1994). Some noteworthy aspects of the Hesston, Kansas, Tornado family of 13 March 1990. Bulletin - American Meteorological Society, 75(6), 1007–1017. https://doi.org/10.1175/1520-0477(1994)075<1007:SNAOTH>2.0.CO;2
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