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The Dexes / Heavy Rain / 693915

Eventdex · Heavy Rain

SMITH

693915 · 39.780, -98.780

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Event typeevent_typeHeavy Rain
NOAA NCEI event IDncei_event_id693,915
Episode IDepisode_id114,793
Begin UTCbegin_utc2017-05-16T12:00:00+00:00
End UTCend_utc2017-05-17T12:00:00+00:00
StatestateKANSAS
County/zone typecz_typeC
County/zone namecz_nameSMITH
Latitudelat39.780
Longitudelon-98.780
End latitudeend_lat39.780
End longitudeend_lon-98.780
Deaths directdeaths_direct0
Deaths indirectdeaths_indirect0
Injuries directinjuries_direct0
Injuries indirectinjuries_indirect0
Damage propertydamage_property0.00K
Damage cropsdamage_crops0.00K
Weather forecast office sourcewfo_sourceCoCoRaHS
Episode narrativeepisode_narrativeThunderstorms produced damaging winds and some severe sized hail over several counties in north central Kansas on this Tuesday evening. Scattered single cell thunderstorms began developing around 3 PM CST from central Kansas northeast into southern Nebraska. The formation of numerous cells quickly resulted in a transition to a multicell convective mode by 4 PM CST. This nearly continuous line of storms lifted north into Nebraska by 530 PM CST. As these storms affected north central Kansas, low-end severe hail occurred from southwest to northeast across Rooks, Osborne, and Jewell Counties. The strongest winds were west of this swath. Phillips County was hit particularly hard as measured wind gusts reached 75 mph in Logan and 71 mph at Phillipsburg. In Phillipsburg, large tree branches were snapped off, knocking out power. The roof was also blown off a restaurant. Scattered thunderstorms continue to develop and move into north central Kansas, at times through the evening and overnight hours, and even into Wednesday morning. None of them were severe until a multicell cluster formed over Lincoln County around 530 AM CST. As this cluster lifted north across Mitchell County, between 645 and 745 AM, they produced 1 inch hail. Other scattered storms developed across the rest of north central Kansas, during the morning hours. They weakened and dissipated, forming a large shield of anvil rain that extended into south central Nebraska. As this rain shield began to dissipate, conditions became favorable for a wake low to form. This resulted in a wind gust of 61 mph at Smith Center, at 1015 AM CST. Repeated thunderstorm activity resulted in swaths of 2 to 3 inches of rain. The highest amount was 3.80 inches in Smith Center.||Low pressure was over South Dakota, and its trailing weak cold front moved into south central Nebraska during the day. It became stationary as low pressure formed over southeast Colorado and deepened to near 990 mb. In the upper-levels, a longwave trough was over the Western U.S. with a ridge over the East. A strong shortwave trough lifted out of the Desert Southwest into the Southern Plains, while a closed low dropped into the Pacific Northwest. In the preconvective environment, an elevated mixed layer had overspread a moist boundary layer. Mid-level lapse rates were between 8 and 9 C/km. MUCAPE was between 3000 and 4500 J/kg. With strong dynamic forcing, deep layer shear was very strong, between 40 and 60 kt.
Event narrativeevent_narrativeA 24 hour rainfall total of 3.63 inches was reported.
Yearyear2,017

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SMITH — Heavy Rain — TerraPulse