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<br />high-intensity storm that culminated several days of widespread gen- <br />eral rain. Precipitation began on June 28 and continued until July 3, <br />when 3 inches fell in a 3-hour period atthe Weather Bureau rain gage <br />in the village of Elm Creek, The village is about 13 miles downstream <br />from the three gaging stations where peak discharges were measured <br />(table 23), The amount of rainfall on July 3 at surrounding rain <br />gages is given in figure 30. It is not known whether the amount of rain <br />that fell on the basin above the gaging stations was greater or less <br />than that at the village. The recurrence interval of a 3-inch rainfall <br />in 3 hours at this site is about 25 years, according to the U.S. Weather <br />Bureau (1961). <br />The peak discharges at ,all three gaging stations were maximum <br />during the 15-year period of record. That on Elm Creek near Sumner <br />(sta,2) was 'about 6 times the previous maximum pE1ak and had a re- <br />currence interval much greater than 50 years, The peak discharges on <br />the tributaries that enter Elm Creek about 1 mile upstream (sta. 1) <br />and 0.5 mile downstream (sta. 3) from station 2 were from about 1% <br />times to 2 times that of the previous maximum discharges and had re- <br />currence intervals of more than 50 years. Damage from the flood was <br />slight and consisted mostly of hank and streambed erosion. <br />Rock Creek 'in south-central Dundy County (fig. 31) flooded on <br />July 3 and 5, each time following cloudburst-type rainfall, After the <br />first downpour, a few local residents reported that their rain gages in- <br />dicated about 8 inches, and several others reported that their 5-inch- <br />oopacity gages had overflowed, The second storm not only dumped <br />another 3 inches on the ltlready wet ground but was accompanied by <br />hail that caused much damage to crops. <br /> <br />E68 <br /> <br />FLOODS OF 19'65 IN THE UNITED STATES <br /> <br />S~Y OF FLOODS <br /> <br />'rrigated land required releveling. Many rural structures, much farm <br />~uipment, and many irrigation facilities w~re demolished, a~d about <br />75 head of livestock were lost, Several mIles of road repaIrs were <br />necessary, and at least 10 bridges needed repair or replacement. The <br />following table of flood damage was farmshed by the Corps of <br /> <br />Engineers: <br /> <br />Type 01 damage <br />Urban and suburban_____________ <br />Rural __________________________ <br />Transportation facilities__________ <br />Business _______________________ <br />Emergency costs_________________ <br /> <br />Losses <br /> <br />$170,000 <br />954,000 <br />260,000 <br />426,000 <br />40,000 <br /> <br />Total _________n_________ 1,850.000 <br /> <br />FLOODS OF JULY IN NEBRASKA <br /> <br />By H. D. BRICE <br /> <br />Intense precipitation caused exceptionally high discharges on five <br />Nebraska streams during July 1965. The recurrence intervals for the <br />peak discharges are all greater than 50 years. . <br />Flooding on July 3 in the upper part of the Elm Creek dramage <br />basin in eastern Dawson County (fig, 30) resulted from a localized <br /> <br />99' <br /> <br />,Ooonto6SWl.5' ~~ <br />Area of report <br /> <br />EXPLANATION <br />.' <br />Flood-determination point <br />Numbe.. corresp<mds to <br />t/u;ttintable!l!J <br />"Oconto 6 SW 1.53 <br />Precipitation measurement site <br />showing number of miles in in- <br />dicated direction from town and <br />amount of rainfaU, in inches, <br />on July 3 <br /> <br />No. Stream and place of deter- <br />mination <br /> <br />". <br /> <br /> <br />TABLE 23.-Flood stages and discharges, July, in Nebraska <br /> <br /> <br />s8mner <br /> <br />Maximum fioods <br /> <br />nminage <br />area <br />(sqmi) <br /> <br />Known before <br />IDly 1965 July 1965 <br />Period Year <br /> <br />b~~ <br />(feet) <br /> <br />Platte River basin <br /> <br />1 Elm Creek tributary near <br />Overton. ........hhhh.. <br />2 ElmCreeknearSumner____. <br />3 ElmCreektributar'yNo.2 <br />near Overton._u__________ <br /> <br />0.54 __~=:~~_m~:~h"------3- <br />14.9 19.51-65 19.58 ______Ud <br />3 <br />3 <br /> <br />13.59 <br />13.74 <br />'HI <br />14.76 <br />114.63 <br />13.13 <br /> <br />Lexington <br />7 ESE 0.91 <br />, <br /> <br />K~arney 1.30 <br /> <br />5.19___________________ <br />1951-66 1961 <br /> <br />> <br />Canaday stream <br />plant 1.06 <br /> <br />iver <br /> <br />Kansas River b.sin <br /> <br />5 <br />I <br /> <br />SMILES <br />I <br /> <br />__~~____~~~__n------3- <br />5 <br />19 <br /> <br />o <br />, <br /> <br />4 Rock Creek at Parksh_mn <br /> <br />180 <br />'14 <br /> <br />FIGURE 3O.-Location of flood-determination points and precipitation stations, <br />floods of .July 3 in sOuth.central Nebraska. <br /> <br />5 Big Blue River at Surprise___ <br /> <br />345 <br /> <br />1 Datum changed; relation to previously published recordS unknOwn. <br />2 Contributing drainage area. <br /> <br />E69 <br /> <br />Discharge <br />Cfs Ratioto <br />Q,o <br /> <br />142 _._hhU_ <br />206 1.32 <br />271___n_____ <br />1,660 2.55 <br />679 L64 <br />307 _______n_ <br /> <br />U7 <br />'48 <br />.00 <br />.L02 <br /> <br />110__._______ <br />300 L<4 <br />433 LM <br />10,900 1.15 <br />