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contributor authorKane, Richard J.
date accessioned2017-06-09T14:44:38Z
date available2017-06-09T14:44:38Z
date copyright1991/03/01
date issued1991
identifier issn0882-8156
identifier otherams-2575.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162567
description abstractTwo tornado events and an intense downburst episode were investigated in an attempt to relate cloud-to-ground lightning rates with the occurrence of severe local storms. The State University of New York at Albany lightning detection system was used to yield characteristic lightning rate tendencies and particular lightning signatures that were associated with severe storms in the northeastern United States. Tornadoes and large hail occurred about 10?15 min after a pronounced peak in the 5-min cloud-to-ground lightning rate. In the downburst event, very destructive winds occurred just after the 5-min rate peaked. Because these severe local storm activities followed well-defined peaks in the 5-min cloud-to-ground lightning rate, it may be possible that the 5-min rates could be used operationally to forecast severe weather.
publisherAmerican Meteorological Society
titleCorrelating Lightning to Severe Local Storms in the Northeastern United States
typeJournal Paper
journal volume6
journal issue1
journal titleWeather and Forecasting
identifier doi10.1175/1520-0434(1991)006<0003:CLTSLS>2.0.CO;2
journal fristpage3
journal lastpage12
treeWeather and Forecasting:;1991:;volume( 006 ):;issue: 001
contenttypeFulltext


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