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<br />at Brownville, Nebraska, was more than 4.5 feet above flood stage. Based upon <br />data collected at the Missouri River gage at Nebraska City, Missouri River flows <br />likely approached 100,000 cfs at the mouth of the Nishnabotna River, while that <br />river was near peak stage. <br /> <br />J <br /> <br />The peak stage of 33,2 feet reached by the Nishnabotna River at Hamburg <br />gage set a new record stage at this station. This exceeds the previous record flood <br />stage of 30.56 feet set on 25 July 1993. Station records go back to 1923. Since <br />the final discharge estimate is not available yet, a frequency has not been assigned <br />to the flood. Based upon the discharge measurement made at Riverton, the flood <br />definitely exceeded the 1 DO-year event, <br /> <br />; <br /> <br />Flooding continued on the lower Nishnabotna River and the Missouri River <br />from Nebraska City downstream through the end of June, as flood water returned <br />to the channel from flooded fields. Thunderstorms continued to pound other parts <br />of the District as a cold upper-level storm system moved from the northern Rockies <br />onto the northern Plains. Heavy rains of 2.5 to as much as 5 inches fell in <br />northeast Nebraska and in the Dakotas on June 17th and 18th resulting in some <br />lowland flooding, particularly on Shell and Beaver Creeks west of Columbus, <br />Nebraska. Reservoir elevations in the Black Hills rose in response to runoff from <br />those storms. Snow accumulated in the high mountain passes from Colorado <br />through Montana. Minor flooding was also reported in the Beaverhead River basin <br />of Montana, due to above normal rainfall and seasonal snowmelt on the 19th. <br /> <br />(5) Early Summer 1998. <br /> <br />, <br /> <br />Widespread thunderstorm activity returned to the northern plains by <br />June 23'd, as thunderstorms developed north of an upper level high-pressure ridge <br />centered over Texas. Thunderstorms became more numerous along the Front <br />Range as the circulation around the high-pressure system set up a monsoonal <br />moisture flow in eastern Colorado, Wyoming and Montana. Two to four inches of <br />rain fell in the South Platte River basin northeast of Denver on the 23'd, with <br />tornadoes and hail reported in Wyoming and several locations in Nebraska. Flash <br />flooding was reported along small streams in northwest Iowa and northeast <br />Nebraska on the 24th. Minor flooding occurred along Pebble and Maple Creeks <br />northwest of Fremont, Nebraska, the Boyer River near Denison, Iowa, and the West <br />Fork Ditch near Hornick, Iowa. The Missouri River pushed above flood stage at <br />Williston, North Dakota, and the Cheyenne River rose to near flood stage at Cherry <br />Creek, South Dakota, <br /> <br />, <br /> <br />Montana became the focus of storm activity by June 26th. Two to 4 inches <br />of rain added to receding snowmelt runoff and caused flooding of minor streams <br />near Dillon and on the Ft. Belknap Indian Reservation. Continued rain caused larger <br /> <br />15 <br />