This tornado also was obscured by rain for much of its life cycle, but was documented at close range by Doppler on Wheels (DOW) research scientists. The second tornado of this storm began 3 miles northeast of American Horse Lake, or 9 miles west-northwest of Geary. It appeared to weaken/dissipate as it crossed Highway 54 about 6.5 miles south-southeast of Thomas, where several power poles were snapped.
The tornado was wrapped in rain for much of its existence. This tornado began 4.5 miles south of Thomas, and touched down intermittently as it moved east-southeast. The first 10 tornadoes during the event occurred in the NWS Norman county warning area in Blaine, Canadian, Custer, Kingfisher, Lincoln, Logan and Oklahoma Counties. Note: All 16 tornadoes that occurred during the afternoon and evening of May 29th and the early morning of May 30th in Oklahoma were produced by the same parent supercell thunderstorm. NWS Norman Product and Event Chronology for May 29, 2004ĩ WNW Geary - 2.5 N Geary - 9.2 NNW Calumet (11 W Okarche)ġ0.3 WNW Edmond - 7.1 NW Edmond (just N of Council/NW 206 - just E of Portland/Sorghum Mill) Numerous reports of tornadoes were received from the region, including the states of Kansas, Missouri, Nebraska, and South Dakota as depicted in the Storm Prediction Center's preliminary storm reports map for May 29-30, 2004.Ī summary of each tornado generated by this supercell thunderstorm can be found within the Tornado Data tab. The supercell that traversed Oklahoma was part of a larger outbreak of severe weather that occurred On May 29-30, 2004, in the central Great Plains. It took a track similar to, and just north of the track taken by another cyclic supercell that had occurred slightly more than a year earlier on May 9, 2003. The supercell produced 10 tornadoes in NWS Norman area and another 6 tornadoes in the NWS Tulsa area in northeastern Oklahoma. The supercell would move through northeastern Oklahoma, including the Tulsa metropolitan area, before dissipating just east of the Arkansas state line in Delaware County during the early morning hours of May 30, 2004. The storm continued to produce large hail, high winds, and/or tornadoes through northern Lincoln and southern Payne counties before moving into Creek County and leaving the NWS Norman area of responsibility by 11:30 PM CDT (10:30 PM CST). The supercell tracked through Custer, southern Blaine, northern Canadian, southern Kingfisher, northern Oklahoma, and southern Logan counties, just skirting the northern Oklahoma City metro area. Most of the other storms either dissipated or moved northward into Kansas, leaving this particular supercell as the dominant storm in Oklahoma during the late afternoon and evening hours. The supercell formed in western Oklahoma within a line of thunderstorms that initiated near the dry line. and State College, Pa.During the afternoon and evening of May 29, 2004, a cyclic supercell thunderstorm moved through west-central and central Oklahoma producing tornadoes, large hail, and high winds. Portland, Me., Lewiston, Me., Bangor, Me., Ogunquit, Me., Burlington, Vt., Essex, Vt., Manchester, Nh., Concord, Nh., Nashua, Nh., Boston, Ma., Worcester, Ma., Springfield, Ma., Bridgeport, Ct., New Haven, Ct., Hartford, Ct., New York, Ny., Hempstead, Ny., Brookhaven, Ny., Buffalo, Ny., Rochester, Ny., Newark, Nj., Jersey City, Nj., Paterson, Nj., Elizabeth, Nj., Trenton, Nj., Providence, Ri., Warwick, Ri., Philadelphia, Pa., Pittsburgh, Pa., Allentown, Pa. Provide: Northeast Live Doppler Radar and Weather Forecasts for Major Cities within the Northeastern US. For additional information please contact: Forecast Ticker can be licensed for use on other websites or blogs, the ticker size and or colors can be modified to fit any theme. The Interactive Live Northeastern Weather Forecasts ticker is updated hourly by the Weather Information Network and provides a scrolling snapshot of current weather conditions for cities in the Northeastern region of the U.S.
Northeast doppler radar 1800 mile update#
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