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contributor authorMcCaul, Eugene W.
contributor authorBuechler, Dennis E.
contributor authorHodanish, Stephen
contributor authorGoodman, Steven J.
date accessioned2017-06-09T16:14:12Z
date available2017-06-09T16:14:12Z
date copyright2002/02/01
date issued2002
identifier issn0027-0644
identifier otherams-63890.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4204942
description abstractThe visual, radar, and lightning characteristics of a severe thunderstorm that spawned a large F3 tornado near Almena, Kansas, on 3 June 1999 are documented. The storm is interesting in that it made a transition from a low-precipitation to classic supercell then back to low-precipitation supercell again prior to dissipation after sunset. The storm remarkably produced only 17 cloud-to-ground lightning flashes during its 4.5-h lifetime, despite vertically integrated liquid (VIL) values reaching 95 kg m?2, reflectivities of 50 dBZ or greater at altitudes of 14 km, and baseball-size hail at the surface. In contrast, total lightning rates inferred from a portable lightning detector during the large tornado were very high, approximately 100 per minute, as expected for a storm of this size and intensity.
publisherAmerican Meteorological Society
titleThe Almena, Kansas, Tornadic Storm of 3 June 1999: A Long-Lived Supercell with Very Little Cloud-to-Ground Lightning
typeJournal Paper
journal volume130
journal issue2
journal titleMonthly Weather Review
identifier doi10.1175/1520-0493(2002)130<0407:TAKTSO>2.0.CO;2
journal fristpage407
journal lastpage415
treeMonthly Weather Review:;2002:;volume( 130 ):;issue: 002
contenttypeFulltext


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